i! P- CD i ru i CD a m CD MICROBIOLOGY MARSHALL MICROBIOLOGY A TEXT-BOOK OF MICROORGANISMS GENERAL AND APPLIED CONTRIBUTORS F. T. Bioletti, Berkeley, California. R. E. Buchanan, Ames, Iowa. M. Dorset, Washington, D. C. S. F. Edwards, Guelph, Canada. W. D. Frost, Madison, Wisconsin. F. C. Harrison, Macdonald College, Canada. E. G. Hastings, Madison, Wisconsin. H. W. Hill, Minneapolis, Minnesota. W. E. King, Detroit, Michigan. J. G. Lipman, New Brunswick, N. J, W. J. MacNeal, New York City E. F. McCampbell, Columbus, Ohio. Earle B. Phelps, Boston, Massachusetts. Otto Rahn, East Lansing, Michigan. M. H. Reynolds, St. Paul, Minn. W. G. Sackett, Fort Collins, Colo. W. A. Stocking, Ithaca, New York. Charles Thorn, Starrs, Connecticut. J. L. To'dd, Montreal, Canada. EDITI;D i;v CHARLES E. MARSHAL'. Amherst, Massachusetts PROFESSOR OF MICROBIOLOGY AND DIRECTOR OF GRADUATE SCHOOL MASSACHUSETTS AGRICULTURAL COLLEGE WITH 128 ILLUSTRATIONS PHILADELPHIA P. BLAKISTON'S SON & CO. 1012 WALNUT STREET 1912 COPYRIGHT, 1911, BY P. BLAKISTON'S SON & Co. Reprinted with Corrections, June 1912 THE. MAPLE. PRESS- YORK PA CONTRIBUTORS. BIOLETTI, FREDERIC T., M. S. Associate Professor of Viticulture, University of California, Berkeley. Viti- culturist of Experiment Station. BUCHANAN, R. E., PH. D. Professor of Bacteriology, State College, Ames, Iowa. Bacteriologist of Expe ment Station. DORSET, M., B. S., M. D. Chief of Biochemic Division, U S. Bureau of Animal Industry, Washing- ton, D. C. EDWARDS, S. F., M. S. Professor of Bacteriology, Ontario Agricultural College, Guelph, Canada. FIDLAR, EDWARD, B. A., M. B. Director of City Laboratories of Pathology and Public Health, City Hospital, Hamilton, Ont., Canada. FROST, W. D., PH. D. Associate Professor of Bacteriology, University of Wisconsin, Madison. HARRISON, F. C., D. Sc., F. R. S. C. Principle, Professor of Bacteriology, Macdonald College (Faculty of Agricul- ture, McGill University), Quebec, Canada. HASTINGS, E. G., M. S. Associate Professor of Agricultural Bacteriology, University of Wisconsin, Madison. Bacteriologist of Experiment Station. HILL, H. W., M. B., M. D, D. P. H. Director: Division of Epidemiology, Minn. State Board of Health. Assistant Professor of Bacteriology, University of Minnesota, Minneapolis. KING, WALTER E., M. A. Formerly Professor of Bacteriology, Agricultural College, Manhattan, Kansas. Bacteriologist of the Experiment Station. Asst. Director, Research Laboratory, Parke, Davis and Co., Detroit, Mich. LIPMAN, JACOB G., PH. D. Professor of Soil Fertility and Bacteriology, Rutgers College, New Brunswick, New Jersey. Director, Soil Chemist and Bacteriologist of Experiment Station. Note Edward Fidlar, B. A., M. B., Senior Demonstrator of Pathology and Bacteriology in the University of Minnesota, cooperated with Dr. H. W. Hill in the preparation of the account of specific diseases. V VI CONTRIBUTORS. MACNEAL, W. J., M. D., PH. D. Lecturer on Pathology and Bacteriology, New York Post-Graduate Medical School. MCCAMPBELL, E. F., S. B., Ph. D., M. D. Secretary of State Board of Health of Ohio; Professor of Bacteriology, Ohio State University. PHELPS, EARLE B., S. B. Assistant Professor of Research in Chemical Biology, Massachusetts Institute of Technology, Boston. RAHN, OTTO, PH. D. Assistant Professor of Bacteriology, Michigan Agricultural College, East Lansing. Assistant Bacteriologist, Experiment Station REYNOLDS, M. H., B. S., M. D., D. V. M. Professor of Veterinary Medicine, Agricultural College, University of Minnesota, St. Paul, Minn. Veterinary Medicine and Surgery, Experiment Station. SACKETT, WALTER G., B. S. Bacteriologist of Experiment Station, Colorado Agricultural College, Fort Collins. STOCKING, W. A., M. S. A., Professor of Dairy Industry, Cornell University, Ithaca, N. Y. Dairy Bacteri- ologist of Experiment Station. THOM, CHARLES, PH. D., Mycologist, Dairy Division, Bureau of Animal Industry, U. S. Dept. of Agri- culture, Stationed at Storrs, Conn. TODD, J. L., M. D., D. Sc. Associate Professor of Parasitology, McGill University, Montreal Canada Dr. L. F. Rettger of Yale University kindly furnished a brief review of "Bacillary White Diarrhoea of Chicks." INTRODUCTION. By a process of adaptation and growth, the branch of science commonly recognized as "Bacteriology" has for many years included, besides the bacterial forms, those microorganisms yielding to the same laboratory methods of study and investigation. This is a policy or purpose instituted by Pasteur. It is also the result of investigations and added knowledge, more definite arrangements of available facts, and the highly specialized training required for the work. In short, technic together with the eco- nomic relations of the subject-matter has no little influence in placing limitations. In the light of such circumstances, it appears more pertinent to designate this text-book as "Microbiology," perhaps not the best term, but one much in accord with French usage. Agriculture, Domestic Science and certain other courses in scientific schools and colleges call for the treatment of the subject in such a man- ner as to make it basic to the interpretation of such subjects as air im- purities, water supplies, sewage disposal, soils, dairying, fermentation industries, food preservation and decomposition, manufacture of biolog- ical products, transmission of disease, susceptibility and immunity, sani- tation, and control of infectious or contagious diseases. A strong effort has been made to provide the fundamental and guiding principles of the subject and to show just how these principles fit into the subjects of a more or less strictly professional or practical nature. Here the instruc- tional work of the microbiologist stops in most educational institutions and the instruction of the practical or professional man begins. Because of the extreme massiveness and diversity of the subjects, Agriculture and Domestic Science and Industrial Vocations in general, a comprehensive consideration of the subject is demanded. Elimination of many features not only becomes difficult but really precarious, because so many avenues are open to the student that pertinency cannot always be foreseen or determined. It is well to remember, too, that such aggre- gate subjects as Agriculture and Domestic Science, unlike Engineering and Medicine, because of their youth, have not developed to that stage VII Vlll INTRODUCTION. in their educational history where practice and the science upon which practice should be founded are amalgamated. The practical man in Agriculture, and Applied Sciences generally, too frequently is so extremely traditional in his practice that he utterly fails to separate the true from the false, or, in other words, does not exercise his discriminative powers at all, but depends entirely upon so-called haphazard methods and self- willed processes. This factor operates against the proper development and logical study of any branch of science in its relation to the farmer, or manufacturer. The plan of a text-book in Microbiology which seeks to furnish basic principles, to train the mind in logical development and adjustment, and to prepare the student to undertake an intelligent study of strictly professional or practical subjects, must assume a definite and systematic arrangement. With this in mind, the text has been divided into three distinct parts: Morphological and Cultural, or that which deals with forms and methods of handling; Physiological, or that which deals strictly with functions, the key to the applied; Applied, or that which reaches into the application of the facts developed to the problems met in the study of professional or practical affairs. In a text-book, the product of several hands, there is the most serious difficulty in obtaining unity of thought and expression without repetition; besides, that very conspicuous weakness of emphasizing some features unduly while other features of importance are scarcely mentioned, con- fronts us. A most earnest attempt has been made to overcome these faults as far as possible, but a complete mastery of them cannot be ex- pected in the first product. However, what is lacked in unity and con- tinuity of expression and in balance, we sincerely hope will be made up, in part at least, by the selection and the value of the material contributed. Laboratory features of microbiology have been eliminated wher- ever it has been practicable. Should any demonstrations be added or needed, we have felt that they may be easily supplied by the instructor, who, of course, will be governed by local facilities and conditions. Al- though no space has been given to laboratory exercises, it should not be gathered that the authors of this book are any the less earnest in urging a well-organized laboratory course to supplement the general instruction as an essential factor to a working appreciation of the subject. In matters of spelling, new words, and phrases, conservatism has controlled. Arbitrary decisions and selections have been forced in INTRODUCTION. IX several instances to secure clearness, consistency and definiteness. It is painfully evident to anyone attempting to bring system out of the confusion and chaos existing in many fields of microbiological action that some rearrangement ought to be undertaken. As usual, however, this will be very slow on account of the many almost insurmountable difficulties. We need and invite helpful suggestions and criticisms at all times, for a valuable text-book of the nature of this is one of slow growth and development and not of " sport evolution." The editor is certain that each contributor will welcome suggestions and, further, will be in far better position to judge his own contribution after the material appears in book form and has been submitted to students for which it is designed. No one better than the editor realizes fully the sympathetic part played by the contributors. If any merit attaches to this book as it finds its place in microbiological instruction, such merit should be recog- nized as due the contributors whose unselfish aims have made it possible. CHARLES E. MARSHALL, EDITOR. EAST LANSING, MICHIGAN. CONTENTS. TITLE PAGE iii CONTRIBUTORS v INTRODUCTION (Editor) vii CONTENTS (Editor) ' xi HISTORICAL REVIEW (Harrison) i PART I. MORPHOLOGY AND CULTURE OF MICROORGANISMS. GENERAL (Editor). OUTLINE OF PLANT GROUPS (Thorn). OUTLINE OF PROTOZOAL GROUPS (Todd). CHAPTER I. MOLDS (Thom) 12 Fungi in general, Bacteria, Phycomycetes, Ascomycetes, Basidiomycetes, Imperfect fungi. Molds, Cosmopolitan saprophytes, molds of fermentation, parasites and facultative parasites. Consideration of groups, Mucor, Penicillium, Aspergillus, Cladosporium, Alternaria and Fusarium, Oidium, Monilia, Dematium. CHAPTER II. YEASTS (Bioletti) 28 Morphology of certain types, Definition and bases of classification, general morpho- logical characteristics. The principal yeasts of importance to fermentation indus- tries, True yeasts, pseudo-yeasts. Culture of yeasts. CHAPTER III. BACTERIA (Frost) 37 Form, Fundamental form types, gradations, involution forms. Size. Motility, Brownian movement, vital movement, organs of locomotion, character of move- ment, rate. Reproduction, Vegetative multiplication, spore formation. Cell grouping. Structure of the bacterial cell. Higher bacteria. Classification. Rela- tionship of bacteria. Cultivation of bacteria. CHAPTER IV. INVISIBLE MICROORGANISMS (Dorset) 64 A brief general discussion of the available knowledge of invisible microorganisms. CHAPTER V. PROTOZOA (Todd) 68 Introduction. Structure of protozoa. Functions of protozoa, Locomotion and reproduction, developmental cycle, encystment. Parasitism. Discussion of classi- fication. Technic. PART II. PHYSIOLOGY OF MICROORGANISMS (RAHN). DIVISION I. NUTRITION AND METABOLISM. (A Few Paragraphs on Protozoal Nutrition by Todd.) INTRODUCTION, Principles of nutrition and metabolism, energy supply of microorganisms. xi CONTENTS. CHAPTER I. FOOD OF MICROORGANISMS 8 The composition of the cell Moisture, cell wall, cell contents.-Amount of food re- Organic food materials,-Non-nitrogenous food compounds, nitrogenous food compounds.-Mineral food.-Oxygen.-Additional remarks on microbial food - Physiologic groups, synthetic media. CHAPTER II. PRODUCTS OF METABOLISM The chemical equations of fermentations. Physiological variations. Products' from nitrogen-free compounds, Cellulose, starch, sugar, alcohols, organic acids, fats. Pro- ducts from nitrogenous compounds Protein bodies, ptomains, urea, uric acid, hip- puric acid. Products from mineral compounds, -Oxidations, reductions. -Unknown products of physiological significance, Pigments, aromatic substances, enzymes and -Rotation of elements in nature.-Carbon cycle, nitrogen cycle, sulphur cycle phosphorus cycle.-Physical products of metabolism.-Production of heat produc- tion of light. CHAPTER III. MECHANISM OF METABOLISM x , General theory of metabolism, Fermentation (intra- and extra-cellular), katabo- lism and anabolism. Intra- and extra-cellular fermentation.-Decomposition of in- soluble food, properties of enzymes, mechanism of fermentation.-Classincation of enzymes.-Hydrolytic enzymes (enzymes of carbohydrates, enzymes of fats, enzymes of proteins), coagulating enzymes, zymases, oxidizing enzymes, reducing enzymes Additional remarks on the relation of cells and enzymes.-Theory of katabolism - Theory of anabolism Interaction of anabolism and intra-cellular fermentation, reversibility of enzymic action. DIVISION II. PHYSICAL INFLUENCES. CHAPTER I. MOISTURE . Osmotic pressure.-Plasmolysis.-Salt and sugar solutions, colloidal solu'tions. -Des- iccation. CHAPTER II. INFLUENCE OF TEMPERATURE , Optimum temperature. Minimum temperature. Maximum temperature. Bio- logical significance of the cardinal points of temperature. -End-point of fermentation. Freezing. Thermal death-point. Resistance of spores. CHAPTER III. INFLUENCE OF LIGHT AND OTHER RAYS ... I ( >2 Phototaxis. X-rays. Radium rays. CHAPTER IV. INFLUENCE OF ELECTRICITY l66 CHAPTER V. IHFLUENCE OF PHYSICAL STRUCTURE OF THE MEDIUM .... . 167 CHAPTER VI. INFLUENCE OF MECHANICAL EFFECTS .168 Pressure. Gravity. Agitation. DIVISION III. CHEMICAL INFLUENCES. CHAPTER I. STIMULATION OF GROWTH 17I Chemotropism and chemotaxis. CHAPTER II. INHIBITION OF GROWTH .173 Poisons, germicides, disinfectants, antiseptics, preservatives. Mode of action. Fac- tors influencing disinfection. Classification of disinfectants. DIVISION IV. MUTUAL INFLUENCES. SYMBIOSIS. METABIOSIS. ANTIBIOSIS .!8i CONTENTS. Xlll PART III APPLIED MICROBIOLOGY. DIVISION I. MICROBIOLOGY OF AIR (Buchanan). CHAPTER I. THE MICROORGANISMS OF THE AIR AND THEIR DISTRIBUTION 185 Microorganisms present in the air. Occurrence in the air. How microorganisms enter the air. Conditions for subsidence of bacteria. Determination of the number of bacteria in the air. Number of bacteria in the air. Species of organisms in the air. CHAPTER II. MICROBIAL AIR INFLUENCE IN FERMENTATION, DISEASES, ETC 19 Air as a carrier of contagion. Organisms of the air and fermentation. Freeing air from bacteria. DIVISION II. MICROBIOLOGY or WATER AND SEWAGE. CHAPTER I. MICROORGANISMS IN WATER (Harrison) 192 Classes of bacteria found in water, Natural water bacteria, soil bacteria and surface washings, intestinal bacteria usually of sewage origin. The number of bacteria in rain , snow, hail, etc., and in water from wells, up-land, surface waters, rivers, and lakes. Causes affecting the increase and decrease of the number of bacteria in water, Tem- perature, light, food supply, oxidation, vegetation and protozoa, dilution, sedimenta- tion, other causes. Interpretation of the bacteriological analysis of water, Quantita- tive standards, qualitative standards. Sedimentation, filtration and purification of water, Sedimentation and filtration, coagulation basins and filtration, porous filters, purification by ozone, purification by heat, purification by chemicals. Location and construction of wells. CHAPTER II. MICROBIOLOGY OF SEWAGE (Phelps) 212 Bacterial flora of sewage. Types of sewage bacteria, Putrefactive and anaerobic bacteria (the liquefaction of protein, the fermentation of cellulose, the saponification of fats, the fermentation of urea, the reduction of sulphates and nitrates), oxidizing bacteria (the production of nitrates and nitrites, other oxidizing reactions) , patho- genic bacteria (prevalence and longevity, life in septic tanks and filters). The culti- vation of sewage bacteria, Filters, anaerobic tanks. The destruction of sewage bacteria, By biological processes, by chemical processes. DIVISION III. MICROBIOLOGY OF SOIL (Lipman). CHAPTER I. MICROORGANISMS OF THE SOIL AS A FACTOR IN SOIL FERTILITY 226 Introduction. The soil as a culture medium; Moisture relations, The amount and distribution of rain fall, range of soil moisture, effect of drouth and exces- sive moisture. Aeration, Mechanical composition of soils, aerobic and anaerobic activities, rate of oxidation of carbon, hydrogen and nitrogen, the mineralization of organic matter. Temperature, Influence of climate and season, early and late soils, production and assimilation of plant food. Reaction, Range of soil acidity, causes of soil acidity, effect of reaction on number and species.- Food supply, Or- ganic matter, the mineral portion of the soil. Biological factors, Molds, algae, proto- zoa, higher plants, bacteria, (numbers and distribution, bacteria in productive and unproductive soils, distribution at different depths, morphological and physiological groups). Methods of study, Quantitative relations, qualitative reaction, transforma- tion reactions, rate of oxidation of carbon, rate of oxidation of nitrogen, addition of nitrogen, reactions concerning calcium, magnesium, sulphur, phosphorus. CHAPTER II. DECOMPOSITION OF ORGANIC MATTER IN THE SOIL 246 Carbohydrates, Origin, decomposition of cellulose, the production of methane and hydrogen, oxidation of methane, hydrogen, and carbon monoxide, the cleavage and fermentation of sugars, starches, and gums. Fats and waxes, Origin and decomposi- XIV CONTENTS. tion. Organic acids, Sources, transformation and accumulation. Protein bodies, Amount and quality, carbon-nitrogen ratio. Transformation of nitrogen compounds, Ammonification, nitrification, denitrification. Analytical and synthetical reac- tions, Amount of bacterial substance in the soil, availability of bacterial matter, transformation of peptone, ammonia, nitrate, nitrogen. CHAPTER III. FIXATION OF ATMOSPHERIC NITROGEN. (Methods of Soil Inoculation by Edwards.) 268 The source of nitrogen in soils, Early theories, chemical and biological relations. Non-symbiotic fixation of nitrogen, Historical, anaerobic species, aerobic species, energy relations. Symbiotic fixation, -Historical, modes of development, resistance, immunity, and physiological efficiency, mechanism of fixation, variations and special- ization, relation to environment. Soil inoculation, Methods of soil inoculation, inoculation with legume earth, inoculation with pure cultures. (Edwards). CHAPTER IV. CHANGES IN ORGANIC CONSTITUENTS 284 Weathering process, Origin and formation of soil, influence of biological factors. Lime and magnesia, Removal and regeneration of carbonates, lime as a base, effect of calcium, magnesium compounds upon bacterial activities. Phosphorous, Availa- bility of phosphates, relation of phosphorus to decay and nitrogen-fixation. Sul- phur, Sulphur compounds in the soil, sulphur bacteria, sulphate reduction. Potas- sium, The transformation of potassium compounds in the soil. Other mineral con- stituents, Iron, aluminum, manganese, and copper. DIVISION IV. -MICROBIOLOGY OF MILK AND MILK PRODUCTS. CHAPTER I. THE RELATION OP MICROORGANISMS TO MILK. (Stocking). (The acid- forming bacteria by Hastings.) 292 Importance of milk as a food. Absorbed taints and odors. Changes due to micro- organisms. Microbial, content of milk, Common milk, special milk, certified milk. Sources of microorganisms in milk, Interior of cow's udder, (healthy udders, diseased udders), exterior of cow's body, atmosphere of stable and milk house, the milker, utensils, water supply. Methods of preventing contamination of milk, Individual cows, care of the cow's body, dust in atmosphere, dairy utensils, the milker. Groups or types or microorganisms found in milk, and their sources, General significance of acid-forming bacteria, groups of acid-forming bacteria (char- acteristics of the Bad, lactis acidi group, characteristics of the B. coli-aerogenes group, characteristics of the Bact. bulgaricus group, characteristics of the coccus group) (Hastings), bacteria having no perceptible effect upon milk, the digesting or peptonizing, pathogenic organisms. Factors influencing the developing of microor- ganisms in milk, Initial contamination, straining, aeration, centrifugal separation, temperature, pasteurization, the use of chemicals. The normal development of microorganisms in milk, Germicidal period, period from end of germicidal action to time of curdling, period from time of curdling until acidity is neutralized, final decomposition changes. Abnormal fermentations in milk, Gassy fermentation, sweet curdling fermentation, ropy and slimy fermentation, bitter fermentation, alcoholic fermentation, other fermentations. The commercial significance of mic- roorganisms in milk, Relation of dirt contamination to germ content. Milk as a carrier of disease organisms, Those microorganisms which are beneficial and detri- mental to health, (acid forms, neutral forms, injurious organisms). Bacteriological analyses of milk. Bacteriological milk standards. The value of bacteriological milk standards and analyses. CHAPTER II. THE RELATIONS OF MICROORGANISMS TO BUTTER (Hastings) 335 Types of butter, Sweet cream butter, sour cream butter. The flavor of butter, Control of butter flavor, kinds and numbers of bacteria in cream, spontaneous ripen- ing of cream, use of cultures in butter making, commercial cultures, use of pure cul- CONTENTS. XV tures in raw cream, use of pure cultures in pasteurized cream, pure cultures in oleomargarine and renovated butter, abnormal flavors of butter. Decomposition processes in butter. Pathogenic bacteria in butter. CHAPTER III. RELATION OP MICROORGANISMS TO CHEESE (Hastings) 346 General. Types of cheese, Acid-curd cheese, rennet-curd cheese. Conditions affect- ing the making of cheese, Quality of milk, tests for the quality of milk, ripening of milk, curdling of milk, manipulation of the curd, ripening of cheese (theories of cheese ripening, present knowledge of causal factors, causes of proteolysis, preven- tion of putrefaction, flavor production in cheese) Abnormal cheese, Gassy cheese, miscellaneous abnormalities of cheese (bitter cheese, colored cheese, putrid cheese, moldy cheese). Specific kinds of cheese, Cheddar cheese, Emmenthaler cheese, Roquefort cheese, Gorgonzola cheese, Stilton cheese, Camembert cheese. CHAPTER IV. RELATION OP MICROORGANISMS TO SOME SPECIAL DAIRY PRODUCTS (Stocking) 363 General. Condensed milk, Sweetened condensed milk, unsweetened condensed milk, concentrated milk, powdered milk. Canned butter and cheese. Special milk drinks made by the action of microorganisms, Kumyss, kefir, leben, yoghurt, artificial buttermilk. Frozen milk. Ice cream. DIVISION V. MICROBIOLOGY OF SPECIAL INDUSTRIES. CHAPTER I. DESICCATION, EVAPORATION, AND DRYING OF FOODS (Buchanan) 374 Factors that bring about changes in dried foods. Inhibition 'of growth of micro- organisms in dried food. Methods of drying, Carbohydrate foods, as fruits, macaroni, vermicelli, copra, syrups, molasses, jellies, jams; fats, as cotton seed, olive, and other oils, etc. ; protein foods, as jerked meat, dried beef, dried fish, pemmican, beef extract, gelatin, somatose, milk, eggs, etc. CHAPTER II. HEAT IN THE PRESERVATION OF FOODS (Edwards) 381 Historical resume 1 . Economic importance, From the standpoint of health and die- tetics, and from the standpoint of commerce. Alteration of foods, Physical changes (appearance, mechanical disintegration), chemical changes (appearance, chemical change, palatability and digestibility), biological changes (vital disorganization, normal flora and fauna). Pasteurization, Economic consideration, specific applica- tion (beer, fruit juices, milk and cream, condensed milk). Sterilization, Economic considerations, specific application (meat, fish, vegetables, and fruits). Controlling factors in successful canning, Cleanliness, soundness of raw material, receptacle, water supply, degree of heat required, storage. Spoliation of pasteurized and ster- ilized goods Chemical, microbiological, detection of spoiled goods. Disposal of factory refuse. CHAPTER III. THE PRESERVATION OF FOOD BY COLD (MacNeal) 395 Introduction. The effects of refrigeration upon foodstuffs in general, Changes during chilling, changes during storage, changes after storage. Refrigeration of certain foods, Meat, fish, poultry, eggs, milk, and butter, fruits and vegetables. Legal control of the cold-storage industry. CHAPTER IV. PRESERVATION OF FOOD BY CHEMICALS (MacNeal) 402 The effects of preservatives upon foods in general, The process of curing, the period of storage, the after-storage changes. The chemical preservation of certain foods, Meats, fish, butter, prepared vegetables, and fruits. The nutritive value of pre- served foods. The effects of food preservatives, Substances which preserve by their physical action, substances which preserve by their chemical action, inorganic food preservatives, organic food preservatives, substances added to foods to improve the apparent quality. The legal control of the preservation of foods by chemicals. CONTENTS. CHAPTER V. MICROBIAL FOOD POISONING (MacNeal) ................ 411 General considerations. Infections of food-producing animals transmissible to man. Human infections transmitted in food. Food poisoning due to the growth of sapro- phytic bacteria in the food, Poisonous meat, sausage, fish, shell fish, milk, cream, cheese, and vegetable food. The chemical nature of food poisons. CHAPTER VI. THE MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS (Bioletti) . 418 Wine: Grape juice, and wine as culture media. The microorganisms found on grapes, (molds, yeasts, pseudo-yeasts, bacteria). Microorganisms found in wine, Aerobic organisms (mycodermse, acetic bacteria) , Anaerobic organisms (slime-forming bac- teria, propionic and lactic bacteria, mannitic bacteria, butyric bacteria). Control of the microorganisms, Before fermentation, during fermentation, after fermentation. Beer: The raw materials and microorganisms of brewing, Grains, yeasts of beer, kinds of beer. Outline of the processes of brewing, Introduction, malting (produc- tion of enzymes), work of enzymes and bacteria, fermentation (work of yeasts), after- treatment. Diseases of beer. Miscellaneous alcoholic beverages: Cider, perry, fer- mented beverages of various fruits, hydromel or mead pombe, ginger beer. Dis- tilled alcohol: Introduction, Uses and sources of alcohol. Methods, Preparation of the sugar solution, (saccharine raw materials, starchy raw materials), fermentation. CHAPTER VII. MANUFACTURE OF VINEGAR (Bioletti) ............... 448 Acetic fermentation, Nature and origin of vinegar, vinegar bacteria. Processes of manufacture, Raw materials, fermentation, starters and pure cultures, apparatus, domestic method, Orleans method, Pasteur method, German method, rotating barrels, after treatment. Diseases. CHAPTER VIII. MANUFACTURE OF OTHER FERMENTED PRODUCTS (Bioletti) ..... 460 Preparation and conservation of food material, Compressed yeast, bread, vegetables, starch, sugar, tobacco. Preservation and conservation of miscellaneous products, Indigo, retting, tanning. CHAPTER IX. MANUFACTURE OF VACCINES (King) ................ 467 Introduction. Active immunizing substances (vaccines), Attenuated viruses, small-pox vaccine, blackleg vaccine, rabies vaccine, Dorset-Miles hog-cholera serum, anthrax vaccines. Other vaccines, Asiatic cholera, bubonic plague, tuberculosis, typhoid fever. Bacterial vaccines (bacterins). CHAPTER X. THE MANUFACTURE OP ANTISERA, AND OTHER BIOLOGICAL PRODUCTS RELATED TO SPECIFIC INFECTIOUS DISEASES (King) .............. 480 Antitoxins, Diphtheria antitoxin, tetanus antitoxin. Other antimicrobial sera, Dorset-Niles anti-hog-cholera serum, antistreptococcic serum, antidysenteric serum, antirabic serum, antigen ococcic serum. Tuberculins, Koch's tuberculin (old) , other tuberculins. Mallein. Suspensions for the agglutination tests. DIVISION VI. MICROBIAL DISEASES OF PLANTS (Sackett). INTRODUCTION .............................. 49 CHAPTER I. BLIGHTS ............................. 492 Stem blight of alfalfa. Bacteriosis of beans. Blight of mulberry. Blight of oats. Pear blight. Tomato blight. Walnut blight. CHAPTER II. GALLS AND TUMORS ........... ....... Sz Crown gall. Olive knot. Fingers and Toes of cabbages (Todd). CHAPTER III. LEAF SPOTS .......................... So6 Spot of the larkspur. Bacterial spot of plum and peach. Leaf spot of sugar beet. CONTENTS. XV11 CHAPTER IV ROTS 508 Black rot of cabbage. Wakker's hyacinth disease. Basal stem rot of potatoes. Soft rot of calla lilly. Soft rot of carrot and other vegetables. Soft rot of hyacinth. Soft rot of muskmelon. Soft rot of the sugar beet. CHAPTER V. WILTS 515 Wilt of cucurbits. Leaf disease of nasturtium. Wilt of sweet corn. Wilt of tomato, egg plant, Irish potato, and tobacco. Additional bacterial diseases. DIVISION VII. MICROBIOLOGY OF THE DISEASES or MAN AND ANIMALS. CHAPTER I. METHODS AND CHANNELS OF INFECTION (McCampbell) 520 Infection defined. Microorganisms of diseases considered and classified, Patho- genic bacteria, pathogenic protozoa, ultra-microscopic microorganisms or viruses. The distribution of pathogenic microbial agents in nature. The occurrence of pathogenic microbial agents upon and in the bodies of healthy animals and man. The manner in which infectious agents enter the body and their sources, Air- borne infections, water-borne infections, infections from soil, infections from food, animal carriers of infection, human carriers of infection, contact infection. The routes by which infectious microorganisms enter the body. Variation in infec- tions. The factors which influence the results of an infection, Virulence, num- ber, avenue, resistance. The exact cause of infections, Soluble toxins, endo- toxins, toxic bacterial proteins. The methods by which infectious microorgan- isms are disseminated. The methods by which infectious microorganisms are eliminated from the body. The effect of infectious microorganisms upon the body, The period of incubation, local reactions, general reactions, metabolism, blood-forming organs, parenchymatous tissues, epithelial and endothelial tissues, erythrocytes and leucocytes, antibody formation. CHAPTER II. IMMUNITY AND SUSCEPTIBILITY (McCampbell) 541 General, Definition, hypersusceptibility or anaphylaxis, predisposition and non- inheritance of infectious diseases. Immunity, Natural immunity and susceptibility (racial immunity and susceptibility, familial immunity and susceptibility, individual immunity and susceptibility). Factors of natural immunity (the protection afforded the body by the surfaces, skin and cutaneous orifices, subcutaneous tissue, the exposed mucous membranes of the body, nasal cavity, mouth, lungs, stomach, intestines, genito-urinary tract, conjunctiva, the protective nature of inflammatory processes, natural antitoxins, natural antibacterial substances, normal hemolysins, normal agglutinins, normal precipitins), acquired immu nity, (active immunity, passive immunity). The origin and occurrance of anti- bodies, Antitoxins, (the mechanism of the neutralization of toxin by antitoxin, unit of antitoxin), lysins and bactericidal substances (the structure of lysins, deviation of complement, the fixation of the complement as a test for anti-bodies), cytotoxins and cytolysins, opsonins and phagocytosis (opsonic index, hemoopso- nins), agglutinins (normal agglutinins, the production of agglutinins, the sub- stances concerned in agglutination, structure of agglutinins and agglutinogens, agglutinoids, the stages of agglutination, hemoagglutinins), precipitins (normal precipitins, mechanism of the formation of precipitins, autoprecipitins and iso- precipitins, the phenomena of specific inhibition, antiprecipitins, the precipitinogen, precipitate, coprecipitins, the forensic use of precipitins). The theories of immu- nity, Noxious retention theory, exhaustion theory, phagocytic theory, Ehrlich's side-chain theory. lHAPTER III. MICROBIAL DISEASES OF MAN AND ANIMALS 576 Diseases caused by molds and yeasts (various authors), Pneumomycosis (Thorn), thrush (Thorn); Dermatomycoses, barbers itch, etc., (Thorn), favus (Thorn); Miscellaneous fungus diseases (Thorn), actinomycosis (Reynolds), mycetoma, XV111 CONTENTS. (Fidlar), mycotic lymphangitis (Reynolds). Diseases caused by bacteria, Botryo- mycosis (Reynolds), gonorrhoea (Fidlar), infectious mastitis (Reynolds), Malta fever (Fidlar), staphylococcic infections (Fidlar), streptococcic infections (Fidlar), pneumonia (Fidlar) , anthrax (Harrison) , bacillary white diarrhoea of young chicks (Rettger), chicken cholera (Harrison), chronic bacterial enteritis (Reynolds), con- tagious abortion (MacNeal), diphtheria (Fidlar), dysentery (Fidlar), fowl diphtheria (Harrison), glanders (Reynolds), influenza (Fidlar), hsemorrhagic septicaemia (Reynolds) , leprosy (Fidlar) , plague (Fidlar) , swine erysipelas (Dorset) , tuberculosis (Reynolds), foot rot of sheep (Dorset), foul brood of bees (Harrison), malignant cedema (Fidlar) , symptomatic anthrax (Reynolds) , tetanus (Fidlar) , typhoid fever (Fidlar), Asiatic cholera (Fidlar). Diseases of unknown cause, (Scarlet fever, measles, German measles, Duke's disease, smallpox, chickenpox, mumps) (Hill), canine distemper (Dorset), cattle plague (Dorset), chicken pest (Dorset), contagious bovine pleuro-pneumonia (Dorset), cowpox (King), horsepox (King), sheeppox (King), dengue (Dorset), foot-and-mouth disease (Dorset), hog cholera (Dorset), horse sickness (Dorset), infantile paralysis (Dorset), louping-ill (Dorset), pellagra (MacNeal), rabies (MacNeal), swamp fever (Reynolds), typhus fever (Dorset), whooping cough (Fidlar), yellow fever (Dorset). Diseases caused by protozoa (Todd), Amcebic dysentery, entero-hepatitis of turkeys, African tick fever, relaps- ing or recurrent fever, yaws, other spirochaetal diseases, syphilis, kala-azar, Delhi boil, sleeping sickness, human trypanosomiases of South America, trypanosomiases, of animals, coccidiosis of rabbits, white diarrhoea of chicks, malaria, red water, miscellaneous protozoal diseases, pebrine, CHAPTER IV. CONTROL OF INFECTIOUS DISEASES (Hill) 691 Principles. Practice. Disinfection. Carriage of infection by biological agents. INDEX OF CONTRIBUTORS 701 INDEX OP ORGANISMS 703 INDEX OF SUBJECTS . 709 LIST OF ILLUSTRATIONS. 1. Jansen's microscope 2 2. Mucor, general 18 3. Mucor, zygospore 19 4. Penicilliiim expansum 26 5. Aspergillus glaucus 23 6. Aspergillus fumigatus, A.nidnlans 23 7. Cladosporium herbarum 24 8. Spores of Alternaria 24 9. Fusarium 24 10. Oidium lactis 26 11. Manilla Candida 27 12. Yeast cell 29 13. Spore-bearing yeast cells 30 14. Wine and beer yeasts 32 15. Wild and pseudo-yeasts 35 16. Types of micrococci 37 17. Types of bacilli 37 18. Types of spirilla 37 19. Involution forms 38 20. The division of bacterial cells 41 21. Mitosis in bacterial cells 41 22. Stages in division of bacterial cells 42 23. The formation of spores 44 24. Location of spores in bacterial cells 44 25. Spore germination 45 26. Division forms of micrococci 46 27. Division forms of bacilli 47 28. Threads of Bact. anthracis 47 29. Capsules (Bact. pneumoniae) 49 30. Plasmolytic changes 50 31. Nuclear division 52 32. Distribution of nuclear substance 51 33. Monotrichous bacteria (Msp. comma) 52 34. Monotrichous bacteria (Ps. pyocyanea) 52 35. Lophotrichous bacteria (Ps. syncyanea) 53 36. Lophotrichous bacteria (Sp. rubrum) 53 37. Peritrichous bacteria (B. typhosus] 53 38. Crenothrix polyspora 55 39. Chlamydothrix hyalina 58 40. Cladothrix dichotoma 59 41. Beggiatoa alba 60 42. Pasteur-Chamberland or Berkefeld filtering apparatus 65 43. Miescher's sac 68 44. Amoeba vespertilio 69 45. Stages in division of Amceba polypodia 72 46. Multiplication of Coccidium schubergi 73 47. Amxba proteus 83 xix XX LIST OF ILLUSTRATIONS. 48. Crystals of bacteriopurpurin 121 49. Carbon cycle 125 50. Nitrogen cycle 126 51. Sulphur cycle 127 52. Action of light on bacteria 162 53. Action of light on molds 163 54. Action of light on mold colonies 164 55. Chemotaxis 171 56. Curve of disinfection 174 57. Influence of filtered water on typhoid fever and Asiatic cholera 197 58. Section of sand filter 205 59. Unglazed porcelain filters 207 60. 6 1, 62. Location of wells on farm 209 63. Construction of model well 210 64. Trickling filter, sand filter, dosing tank, septic tank 223 65. Septic tank . . 224 66. Non-symbiotic nitrogen-fixing organism (B. pasteurianus) 270 67. Non-symbiotic nitrogen-fixing organism (Azotobacter vinelandi) 271 68. Ps. radicicola 275 69. Section through root tubercle 276 70,71,72. Influence of Ps. radicicola 279-281 73. Section of cow's udder 297 74. Bacterial colonies in dust from udder 300 75. Bacterial colonies from cow's hair . 301 76. Bacterial colonies from dust of stable 302 77. Small-top milk pails . 305 78. Ropy cream 324 79. Ropy cream organisms 325 80. Chart of Rochester milk supply 330 81. Gassy cheese 348 82. Cheese from lactic starter 349 83. Influence of lactic organisms on casein degradation 354 84. Swiss cheese 360 85. Kepfir grain . 368 86. Bacteria of slimy wine 424 ' 87. Bacteria of wine diseases 4 2 6 88. Vinegar bacteria 45 89. Vinegar barrel 454 90. Rapid process vinegar apparatus . 457 91. Ps. medicaginis 493 92. Pear blight 497 93. Crown gall 5 2 94. Plasmodiophora brassicce 54 95. 96. Oidium albicans 577 97. Trichophyton tonsurans 98, 99. Actinomyces boms 5^ J 100. Gonococci 101. Bact. anthracis, thread formation 600 102. Bact. anthracis, spores 600 103. Organisms of anthrax in capillaries 602 104. Bact. diphtheria 610 105. Westbrook's types of Bact. diphtherias .611 106. Bact. mallei 618 107. Bact. pestis 625 108. Bact. tuberculosis, branching forms '. 630 109. Bact. tuberculosis, from sputum 630 no. Bact. tuberculosis, in culture 631 LIST OF ILLUSTRATIONS. XXI in. B. tetani, with spores 638 112. B. typhosus 642 113. Msp. comma 646 114. Msp. comma colonies in gelatin 647 115. Kidneys in hog cholera, hemorrhagic points 655 116. Negri bodies 663 117. Amoeba coli 668 118. Spirochceta dentium 670 119. Ornithodoros moubata 671 120. SpirochcEta duttoni 672 121. Treponema pallidum 673 122. Herpetomonas donovani 674 123. Structure of trypanosome 676 124. Trypanosoma gambiense . 676 125. Glossina palpalls 677 126. Malarial parasite in human and mosquito cycles 683 127. Longitudinal section of Anopheles 684 128. Babesia bigemina - 687 Colored Plate. The Malarial parasites ... 683 HISTORY OF MICROBIOLOGY* Geronimo Fracastorio, of Verona, was born in 1484, studied medicine in Padua, and published a work in Venice in 1546, which contained the first statement of the true nature of contagion, infection, or disease organisms, and of the modes of transmission of infectious disease. He divided diseases into those which infect by immediate contact, through intermediate agents, and at a distance through the air. Organisms which cause disease, called Seminaria contagionum, he supposed to be of the nature of viscous or glutinous matter, similar to the colloidal states of substances described by modern physical chemists. These particles, too small to be seen, were capable of reproduction in ap- propriate media, and became pathogenic through the action of animal heat. Thus Fracastorius, in the middle of the sixteenth century, gave us an outline of morbid processes in terms of microbiology. Athanasius Kircher, in 1659, demonstrated the presence of "minute living worms in putrid meat, milk, vinegar, etc."; but he did not describe their form and character, and it is doubtful if he ever saw microorganisms. In the year 1683 Antonius van Leeuwenhoek, a Dutch naturalist and a maker of lenses, communicated to the English Royal Society the results of observations which he had made with a simple microscope of his own construction, magnifying from 100 to 1 50 times. He found in water, saliva, dental tartar, etc., what he termed "animalcula." He described what he saw, and by his drawings showed both rod-like and spiral forms, both of which, he said, had motility. In all probability, the two species he saw were those now recognized as Bacillus buccalis maximus and Spirillum sputigenum. Leeuwenhoek's observations were purely objective and in striking contrast with the speculative views of M. A. Plenciz, a Viennese physician, who in 1762 published a germ theory of infectious diseases. Plenciz maintained that there was a special organism by which each in- fectious disease was produced, that microorganisms were capable of reproduction outside of the body, and that they might be conveyed from place to place by the air. * Prepared by F. C. Harrison. HISTORY OF MICROBIOLOGY. The important role that the compound microscope has played in microbiology calls for something regarding the invention of this instrument an invention which antedates Leeuwenhoek's discovery by nearly 100 years. The first compound microscope was made by Hans Jansen and his son Zaccharias, in 1590, at Middelburg, in Holland. The instrument was composed of two lenses mounted in tubes of iron; a representation of it, made from the original and still kept at Middelburg, is shown in Fig. i. From that date the microscope gradually improved. In 1844 the immersion lens was introduced by Dolland. In 1870 Abbe brought out the substage condenser, which still bears his name. Apo- 6 FIG. i. Longitudinal section of a compound microscope made by Zacharias Jansen (.1590). a, microscope tube; b, objective tube; c, ocular. chromatic lenses and many minor improvements were introduced by the firm of Zeiss about 1880. In 1786 O. F. Miiller (a Dane) first attempted to classify, according to the Linnean system, the various organisms previously discovered, and characterized four or five genera among them, the genus Vibrio, in which, under the terms bacillus, lineola, and spirillum, we recognize forms that correspond with our "bacteria" From the middle of the eighteenth century until well on into the nine- teenth, the history of bacteriology is largely the story of a controversy between those who believed that minute living organisms, such as those above referred to, were produced from inanimate substances, and that their formation was spontaneous. Philosophers, poets, and common people of the most enlightened nations accepted this doctrine down to the eighteenth century. The hypothesis regarding formation was known as that of " spontaneous generation," "heterogenesis," and "abiogenesis." The opponents of this theory denied the possibility of a transition from a lifeless to a living condition, and contended that all life came from pre- existing life a theory aphoristically summed up in the phrase "omne vivum ex vivo." Such was the doctrine of Biogenesis, life only from life. In 1668, Francisco Redi, an Italian, distinguished alike as scholar, HISTORY OF MICROBIOLOGY. 3 poet, physician, and naturalist, expressed the idea that life in matter is always produced through the agency of pre-existing living matter; but the beginnings of the real controversy date from the publication of Needham's experiments in 1745. The English divine boiled some meat extract in a flask, made the flask air-tight, and left it for some days. When the flask was opened, he found in it what he termed "infusoria." He naturally concluded that all life had been killed by boiling; and, as the entrance of fresh life from the outside was prevented by the closing of the flask, he considered that the living infusoria must have originated spontaneously from the inanimate constituents of the broth. Twenty years later Abbe Spallanzani alleged that the development of the infusoria "in an infusion maintained at boiling-point for three-quar- ters of an hour was possible only, provided air, which had not been pre- viously exposed to the influence of fire, had been admitted." Objections were made to these experiments and the controversy went merrily on. Gradually experimental evidence accumulated resulting largely from the work of Franz Schulze, and the discovery by Schroeder and Dusch in 1853, that putrescible fluids will not decay after boiling, if protected from the bacteria of the air by means of a cotton- wool filter or plug; and the epoch-making experiments of Pasteur in 1860, with the now well- known Pasteur flask, showed conclusively that the hypothesis of spontane- ous generation, or abiogenesis, could not be proved. Liebig, the celebrated German chemist, strenuously opposed the theories of Pasteur; his authority and the brilliancy of his expositions influenced the scientific world during the period 1840-1860. To Liebig, fermentation was a purely chemical phenomenon unassociated with any vital process; and he treated Pasteur's results with disdain. : ' Those who pretend to explain the putrefaction of animal substance by the presence of microorganisms," he wrote, "reason very much like a child who would explain the rapidity of the Rhine by attributing it to the violent motions imparted to it in the direction of Bingen by the numerous wheels of the mills of Mayence." Again and again Liebig formally denied the correct- ness of Pasteur's assertions; finally Pasteur challenged him to appear before the Academic Commission to which they would submit their respective results. Liebig, however, did not accept the challenge; the victory was with the French savant. In 1841 Fuchs investigated some blue and yellow milk. He exam- ined it with the microscope and discovered the presence of organisms. 4 HISTORY OF MICROBIOLOGY. He succeeded in cultivating the "blue milk" microbe in mallow slime, and re-developed the blue color in milk by introducing some of his culture. The organisms obtained were sent to Ehrenberg, who named them Bac- terium syncyaneum, now known as B. cyanogenus, Ps. syncyanea and B. synxanthum, a name which is still retained in the literature. Since 1860 the master mind of Louis Pasteur has dominated the realm ' of microbiology. His epoch-making discoveries were largely due to his in- tuitive vision, his skill in device and in the adaptation of means to ends, his prodigious industry, and the enthusiasm and love with which he inspired his associates. Trained as a chemist, his first appointment was to a pro- fessorship of chemistry, and his earliest research dealt with problems in molecular chemistry and physics. On his being elected Dean of the Faculty of Sciences at Lille, he commenced to study fermentation. His work in this field was soon followed by important results: the discovery of the organisms which produce lactic and butyric fermentation, and of anaerobic life, or life which flourishes without free oxygen. He devised an improved method of making vinegar, and demonstrated the presence of the acetic organism which he named Mycoderma aceti. Later he studied the diseases of wine, and discovered that bitterness or greasiness was due to a special ferment, and suggested the heating of wines in closed bottles to a temperature of 60, in order to kill the injurious micro- organisms. This process, since called pasteurization, is now largely used, and makes it possible for manufactures and merchants to keep and export wine without losing its flavor or bouquet. It is interesting in this connection to note that a French confectioner named Appert published, in 1811, his method of preserving fruits, vegetables, and liquors by heating and sealing, and hence may be looked upon as the founder of the packing and canning industry. In 1864-65 the silk districts of that region of France, known as the Midi, suffered such serious losses that the yield of cocoons fell from twenty- six million kilogrammes to four million, which entailed a loss of twenty million dollars and caused widespread distress and poverty. An epidemic had broken out among the silk-worms, the dread disease known as Pebrine. Pasteur was induced to make an investigation as to the best means of combating the epidemic; and, after several years of study, he found the organism causing the disease, suggested remedies, and brought back wealth to the ruined communities, but at the cost to himself of im- paired health and partial paralysis. HISTORY OF MICROBIOLOGY. 5 Pasteur's results were very suggestive; and one outcome of his work was that between 1870 and 1880 several important discoveries were made by other investigators. Prior to the dates mentioned, the mortality from blood poisoning, gangrene, and other infections following operations was extremely high. Surgeons regarded such a result as inevitable, and many agreed with the saying of Velpeau, that "the prick of a pin is the open door to death;" but, in 1860, Joseph Lister, an Edinburgh surgeon, began to study the possible role of microbes in the infection of wounds. By sterilizing his instruments, sponges, ligatures, etc., and using antiseptics, he was able to obtain such a high percentage of recoveries that in two years he saved thirty-four patients out of forty, a percentage unheard of up to that time. Hence the origin of the antiseptic and aseptic methods of surgery. Lister's methods, suggested by the ideas of Pasteur, have rendered possible the marvelous surgery of the present day, banished hos- pital gangrene, and robbed confinement of its terrors. To Lister must also be given the honor of devising the first practical way of obtaining a pure culture of bacteria by means of high dilutions. By using this method, Lister obtained some idea of the different fermenta- tions of milk, such as souring, curdling, etc. He also confirmed the con- clusion of Robert Hall (1874), that milk could be obtained from the animal in a sterile condition, thus proving that the souring of milk was caused by organisms from some external source. In 1872, F. Cohn's System of Classification, based on morphological characters, appeared. He distinguished six genera, micrococcus, bac- terium, bacillus, vibrio, spirillum, and spirochaete; four years later this investigator made the important discovery of endospores (spores formed within cells), and noticed that organisms in this state were more resistant to heat than the rods from which they were derived. This fact was ob- served in the well-known "hay bacillus." In 1871, Weigert succeeded in staining bacteria with picro-carmine; but it was not until 1876 that he used the aniline colors, or dyes, for this purpose, and thus opened up a new field which was exploited with such beautiful results by Ehrlich, Koch, Gram, and others. The staining of microorganisms rendered it possible to obtain pictures of them by pho- tographic methods; the art of photomicrography developed thus rapidly. In 1879, Miquel discovered bacteria which grew or developed at tem- peratures between 65* and 75. He isolated them first from the waters * All temperatures are stated in Centigrade scale, unless otherwise indicated. 6 HISTORY OF MICROBIOLOGY. of the Seine, and subsequently from dust, manure, and other substances. Later researches have shown that these thermophilic organisms play im- portant roles in various fermentations. The ninth decade of the last century was prolific in important bac- teriological events. Discovery followed discovery in rapid succession. In 1880, Laveran, a French military surgeon, discovered the protozoon of malaria; in 1881 Robert Koch introduced the poured gelatin and agar plate, which made it possible to obtain pure cultures without difficulty. Investigators were quick to take advantage of this method; and notable results followed. Eberth and Gaffky discovered the bacillus of typhoid fever, and succeeded in growing it in culture media. In 1882, Loeffler and Schlitz discovered the bacterium which causes glanders; and in the following year Koch isolated the vibrio of Asiatic cholera from the in- testines of cholera patients. In 1883 Klebs described the diphtheria bacterium; and, in 1884, LoefBer grew the organism in pure culture. In 1884, Koch published his results on the etiology of tuberculosis, in a paper which will remain as a classical master-piece of bacteriological research, owing to the difficulty of the task and the thoroughness of the work. Not only did Koch show the tubercle bacterium by appropriate staining methods, but he succeeded in obtaining pure cultures of it and in producing tuberculosis by inoculation with his isolated cultures. In 1885, Nicolaier observed the tetanus bacillus in pus produced by inoculating mice and rabbits with soil; later, in 1889, Kitasato isolated this organism, and showed that the cause of the failure in earlier attempts to isolate it were due to the fact that it could grow only in the absence of free oxygen. The specific infecting agents in pneumonia were discovered by Friedlander and Fraenkel about this time, as were also several organ- isms associated with inflammation and suppuration, such as the Strep- tococcus pyogenes and the Staphylococcus pyogenes, discovered by Rosen- bach, and the green pus germ (Pseudomonas pyocyanea) by Gessard. Whilst these discoveries were taking place, largely in Germany, Pas- teur had been engrossed with his prophylactic studies. In 1880, he dis- covered a method of vaccination against fowl cholera; and in 1881 he published his method of vaccination against anthrax. On a farm at Pouilly le Fort, sixty sheep were placed at Pasteur's disposal; ten of these received no treatment, and twenty-five were vaccinated. Some days afterward the latter were inoculated with virulent anthrax, and also twenty-five which had received no vaccine. The twenty-five non-vacci- HISTORY OF MICROBIOLOGY. 7 nated sheep died; and the twenty-five vaccinated ones remained healthy and in the same state as the ten control animals. This convincing experi- ment was followed by others; and, hi the twenty-five years immediately following the introduction of the method, more than ten million animals were vaccinated in France alone, with excellent results. In 1885, as the result of much animal experimentation, Pasteur related to the Academy of Sciences his discovery of a method of vaccination against rabies, or hydrophobia; and six months after the successful treatment of the first case, 350 persons bitten by rabid dogs were vaccinated. An institute for the preparation of vaccines was built by public subscription and named the Pasteur Institute; and since that date more than thirty similar estab- lishments have been founded in different parts of the world. This eighth decade, so pregnant with discoveries of the utmost im- portance to medicine and surgery, was also notable for its discoveries in agricultural bacteriology. The honor of having been the first to work out the causal relation between a specific microbe and a plant disease belongs to Burrill, who discovered the organism of Fire or Pear Blight; and in 1883 to 1888 Wakker discovered the bacillus which produces the "yellows" of the hyacinth, a disease of considerable economic importance hi Holland. To Beyerinck, Hellriegel, and Wilfarth we owe our earlier knowledge of the development and morphology of the nitrogen-fixing organism which produces the nodules or tubercles on the roots of legumes. In 1888 Winogradsky isolated from soils nitrifying microbes which grew in a medium devoid of all traces of organic matter. During this period, Hansen's investigations along the line of the fermentation industry were most important. He devised methods for securing pure cultures of yeasts starting from a single cell, showed that yeasts produced diseases in beer, and established the method of identifying yeasts by observing their micro- scopic appearance, the formation of ascospores, and the production of films. The tenth decade of the nineteenth century was almost as prolific in discovery as the ninth. In 1890 Behring discovered the antitoxin for diphtheria, as a result of the pioneer work on toxins by Roux and Yersin. ' Five years later, this serum came into general use as a curative; and the efficiency of the treatment is shown by a comparison of the death rate from diphtheria before and after the introduction of the antitoxin. The average annual death rate from diphtheria in eight large cities, during the period 1885-1894, was 9.74 per 10,000 of the population before the use of anti- toxin; and during the antitoxin period of 1895-1904 it was 4.29. 8 HISTORY OF MICROBIOLOGY. The subsequent researches on the constitution of toxins and antitoxins by Ehrlich, Metchnikoff, Madsen, and others have been productive of a better understanding of the problems of immunity. In 1892 Pfeiffer discovered the organism of influenza or grippe; and in 1894 Yersin and Kitasato independently discovered the bacterium of bubonic plague. The now well-known serum diagnosis of typhoid fever, whereby living and motile typhoid bacilli are clumped and lose their motility when placed in the diluted serum of a patient suffering from the fever, was due to the work of Gruber and Durham, and the exploitation of the method by Widal, and dates from 1896. In 1898, Shiga discovered the bacterium of dysentery, and the pos- sible cause of pleuro-pneumonia in cattle was found by Nocard. This latter organism was so minute as to be at the extreme limit of micro- scopic definition, and suggested that other well-known diseases, such as foot-and-mouth disease, are probably caused by ultra-microscopic or- ganisms. This year, Ronald Ross worked out the relation between man, the mosquito, and the malarial parasite, a discovery which at once sug- gested the best means of controlling the disease. In 1905, Schaudinn definitely established the causal agent of syphilis, a spirochaete-shaped organism, which he named the Treponema pallidum, and which had escaped earlier discovery on account of its being refractory to the ordinary staining methods. No one can deny that the progress of microbiology in the last forty years has been extraordinary; but much still remains unknown. The causes of some diseases have not been discovered. Smallpox, scarlet fever, yellow fever, mumps, whooping cough, epidemic infantile paralysis, hydrophobia, and others offer an inviting field to the medical micro- biologist ; and the many problems of soil microbiology call for solution by the agricultural microbiologist. Yet it cannot be said that the laborers ' are few. The record of past achievements is an inspiration; and the knowledge that each discovery was the result of persistent and concentrated effort, may give us of the present day firmer faith and greater strength for work in the broad and inviting field before us. PART I. THE MORPHOLOGY AND CULTURE OF MICRO- ORGANISMS. GENERAL.* Microbiology includes some algcc, a few specific molds, which fall in the realm of pathogenesis (disease production), zymogenesis (fermentation- production), and laboratory manipulations; it deals mainly with yeasts, bacteria, and invisible organisms; it dips deeply into the expanse of pro- tozoa; in short, it is concerned almost wholly with the field of unicellular life. On the one hand, the microbiologist meets the botanist and estab- lishes reciprocal relations with him; on the other hand, he mixes with the zoologist and delves into studies of mutual interest. Primarily, the tecli- nic of the microbiologist together with, in part, the economic bearing of the subject seems to be the determinant factor of limitation. Assuming, therefore, that the province occupied by microbiologists consists of the study of unicellular life-forms, because such limitations have been established by actual studies and investigations, through the instrumentality of microbiological technic, it will be pertinent and clarifying to provide a general graphic outline at the start. By this means the student will be able to locate himself, whether he is just launching or has gotten far out on the troublesome and most fascinating sea of micro- biology. The graphic outlines will always be his ready chart. * Editor. 10 MORPHOLOGY AND CULTURE OF MICROORGANISMS. OUTLINE or PLANT GROUPS.* The following is a diagram of plant groups, showing one scheme of placing the bacteria, yeasts, and molds in relation to other groups. Only a few of the sub-groups can be shown in such a scheme. Schizophyta f Schizomycefes ( fission-fungi}, bacteria. (fission- plants) Tballophyta Phycomycetes j Oomycetes Schizophyceae (fission-algae), blue-green algae. [ Chlorophyceae green algae. Algae Phasophyceae brown algae. [ Rhodophyceas red algae. Characeae. Myxomycetes. f Chytridineae. j Zygomycetes (Mucors). Saprolegniaceae (water fungi). . Peronosporacese (downy I ! mildews). Hemiasci (Monascus). Protoascineae (Saccharo- Fungi i myces, Yeasts). Protodiscineae. Discomycetes. Plectascineae (Aspergillus). Pyrenomycetineae. J Penicillium,Fusarium, Alternaria, [ Oidium, Cladosporium, and others. Rusts Smuts Mushrooms. Ascomycetes Euasci - Imperfect Fungi, Conidia only Basidiomycetes Bryophyta (mosses and liverworts) Pteridophyta (ferns, etc.) Spermatophyta (seed plants). OUTLINE OF PROTOZOAL GROUPS, f Limited on account of economic importance to " A CLASSIFICATION OF THE PATHOGENIC PROTOZOA." For discussion of classification see p. 76. Protozoa Rhizopoda I * Charles Thorn. f Amoeba Amoeba dysenteries Amazba coli A mceba meleagridis A moeba buccalis Plasmodiophora ^ Plasmodiophora brassica t J. L. Todd. OUTLINE OF PLANT AND PROTOZOAL GROUPS. II Spirochceta obermeieri Spiroch- w VS ft// N \ v . is fl,V ' i'i il -^=--=--* xS x vv % " /,',? /-'" \ \\ k *E! I /n> // >V _v V .. * I .llll /w / \x* I W' / v\ \ T. IP / ,"' I f !iiii I *ii " * A*? ' i/i 1 *' i'!n j .!.'/ j '/ vv s v \ \\ '4 / // Kit- FIG. 28. Threads of Bact. anthracis. (After Migula.) in the different cases of fission. These zooglceic masses usually assume the forms of pellicles, but their value as diagnostic features is not great. The formation of zooglcea is very frequently only a stage in the life history of an organism. 48 MORPHOLOGY AND CULTURE OF MICROORGANISMS. MINUTE STRUCTURE OF THE BACTERIAL CELL. The typical cell, such as that of a higher plant or animal, is made up of cytoplasm surrounded by a cell wall. The cytoplasm contains a nucleus. There are also frequently present other evidences of structure in the cy- toplasm, such as nucleolus, polar bodies, etc. In addition to these there may be appendages, such as the cilia or flagella. In the case of the bac- terial cell, we find most of these structures present, such as cell wall, cytoplasm, and appendages, but the nucleus is either wanting or is so modified in form as not to be recognized as an ordinary nucleus. BACTERIAL CELL WALL. Structure. All the bacteria have cell walls and it is these that give rigidity to the cell. These walls are rigid and elastic and are probably made up of two layers, the outer one is able to deliquesce and form capsules, or perhaps zooglcea. The inner part re- tains the elasticity and gives the form to the bacteria. These cell walls are readily permeable to water and it is through them that all of the nourishment of the cell is obtained; that is, there are no openings for the entrance of food or the discharge of by-products, but the in- take and output goes on through the cell wall which is entire. The chemical nature of the cell wall is generally protein in nature and in this respect perhaps resembles the animal cell wall more closely than it does the plant cell wall, though many of the bacterial walls resemble those of molds and some fungi. These cell walls take the ordinary stains with difficulty, or not at all, and it is because they do not stain that they are not seen. The ghost figures, frequently seen, are the walls of dead mother cells from which spores have escaped. Capsules. A considerable number of the bacteria regularly, or under cer- tain conditions, form what are known as capsules (Fig. 29). These are mu- cilaginous envelopes which in width frequently exceed that of the organism itself. In microscopical preparations of bacteria it is important to differ- entiate these from artifacts, since by ordinary staining methods the capsules are not colored but appear as colorless areas surrounding the bacteria. If, due to shrinkage of the bacteria, or other material on the preparation, clear spaces are formed, it is readily seen that these might be confused with the real capsule. It is possible to stain the capsules by special methods; these must be used in order to determine positively the existence of the capsules. The material of which the capsules are composed is derived from the cell itself, probably the result of the deliquescence of the outer BACTERIA. 49 portion of the cell wall. This material is mudn-like and is soluble in water. The bacteria which grow in the bodies of animals frequently con- tain these capsules but fail to show them when grown upon artificial cul- ture media. It is difficult, therefore, to determine whether or not an organism has a capsule by mere examination of cultures. Some culture media, however, do cause a formation of capsules in the case of capsulated bacteria. These are blood serum, sometimes, and milk, usually. Beau- tiful capsules can be obtained by growing such bacteria as the Bact. pneumonia, Bact. capsulation, and Bact. u'elchii in milk cultures. Strept. FIG. 29. Capsules. Baft, pneumcnia (Friedlander). (After Weichselbaum from Frost and McCampbell.) mesenteroides is a bacterium which grows in the syrup of the sugar re- fineries and forms abundant capsules. This organism changes the char- acter of the syrup, and its entrance and growth is frequently the cause of serious loss. Sheath. Among the higher bacteria, such as Crenothrix, there is present a thickened and hardened membrane which is spoken of as a sheath. It forms a tube in which the different cells of the plant are con- tained. This sheath is homologous to the capsule and in it are frequently deposited certain by-products of the cell. In Crenothrix we frequently have iron oxides (p. 55). BACTERIAL CYTOPLASM. The cytoplasm of the bacterial cell is similar to the cytoplasm of other cells except that chemical analyses seem to show that it contains a higher percentage of nitrogen. As viewed under 4 50 MORPHOLOGY AND CULTURE OF MICROORGANISMS. the microscope, in either an unstained or stained condition, it appears as a homogeneous mass filling the entire cell and rarely showing any evidence of structure. Ordinary stains, such as are used in animal and plant histol- ogy, fail to reveal the presence of the ordinary nucleus, the whole cell being usually uniformly stained with those stains ordinarily characterized as nuclear stains. When these stains are applied to some bacteria, particu- larly at certain stages of their growth, certain parts stain more readily than others, and we get either what is known as a bi-polar stain or polar gran- ules. In the first case, the ends of bacilli are stained more deeply than the center so that the cells appear very much as diplococci. This bi-polar stain is characteristic of such organisms as the bacterium of chicken cholera or the bacterium of bubonic plague. The polar granules are frequently seen in the diphtheria bacterium and may be located at the poles and also FIG. 30. Plasmolytic changes. (After A. Fischer.) a, cholera vibrio; b, typhoid bacillus; c, Spirillum undula. (From Novy.) at the center. In this germ and in some others it is possible, by special staining, to give the granules a different color from the rest of the organism. In this case these bodies are spoken of as metachromatic granules. Whether or not the bi-polar stains or the polar granules are evidences of structure or not is an open question, since the results obtained might be explained upon the theory that the cells are plasmolyzed (Fig. 30). As a result of plasmolysis the protoplasm of the cell is drawn away from the cell wall and concentrated in areas which would very well explain the appearances. And it seems likely also that the methods employed in staining might lead to plasmolysis, but the metachromatic granules can hardly be ex- plained upon this supposition. They must be either special protoplasmic structures or reserve food material, and for each of these theories there are able supporters. The cytoplasm of the bacterial cell is slightly refractive. It is color- less except in a few cases in which the green coloring matter, like chloro- phyl, is present, as, for instance, Bact. viride and Bad. chlorinum. In the purple sulphur bacteria, the coloring matter bacteriopurpurin is present. The bacterial cytoplasm contains vacuoles at times. BACTERIA. 51 Nucleus. The question of whether or not the bacteria possess a nucleus is one that has engaged the attention of bacteriologists and biolo- gists for some time. It is very certain that the bacteria do not possess a nucleus in the ordinary sense in which the term is used in animal and plant histology. There are several different views in regard to this matter. One is that the bacterial cell is largely nucleus, and attention has already been called to the fact that cytoplasm stains with what are known as nu- clear stains. But this is not convincing proof that the material of the bac- FIG. 31. i and 2, Bacillus mycoides; 3, B. megatherium; 4, B. radicosus; 5, B. oxalaticus. (After Bohuslaw Rayman and Karel Kruis Jrom Guilliermowd review, Bull. Inst. Past.) terial cell is nucleus. Were this true, however, it would fit in very nicely with the theory of evolution, since evolutionists are desirous of finding a group of organisms with the cell reduced to its simplest form. Another idea is that the nuclear material is widely distributed throughout the bacterial cell and not concentrated into one structure (Fig. 31). Such a view as this is in harmony with Biitschli's work. Zettnow appears to have stained nuclei. Another class of thinkers, in which Alfred Fischer is prominent, believe that the bacterial cell is without a nucleus. This is borne out, to their minds, by the findings that the bacterial cell plasmo- lyzes, that the nucleus of higher animals and plants does not; therefore the bacterial cytoplasm is not nuclear. FLAGELLA. The flagella are protoplasmic threads and, undoubtedly MORPHOLOGY AND CULTURE OF MICROORGANISMS. are attached to the cytoplasm of the cell. Whether these flagella pass through openings in the cell wall, or are attached in some way exteriorly FIG. 32. i, Chromatium okenli; 2, B-actcrium lineola; 3, 4 and 5, sulpho-bacteria; 7, Ophidomonas jenensis; 8 and 9, Spirillum uiuhila; 10, Cladothrix dichotoma. (After Biitschlifrom Guilliermond review, Bull. hist. Past.} x\/ F IG - 33- Microspira comma. Monotrichous bacteria. (After Migula from Schmidt and Weiss.) FIG. 34. Pseudomonas py ocy an ea. Monotrichous bacteria. (After Migula from Schmidt and Weiss.) is a question that cannot be answered definitely. But in either case these flagella possess the property of cytoplasm, i.e., that of irritability, and are not to be considered as analogous to mere levers or oars to BACTERIA. 53 FIG. 35. Pseudomonas syncyanea. FIG. 36. Spirillum nibritm. Lopho- Lophotrichous bacteria. (After Migula trichous bacteria. (After Migula from from Schmidt and Weiss.) Schmidt and Weiss.) FIG. 37. Bacillus typhosus. Peritrichous bacteria. (After Migula from Schmidt and Weiss, and Frost and McCampbell.) 54 MORPHOLOGY AND CULTURE OF MICROORGANISMS. a boat. They are very narrow threads, no one knows how narrow since they cannot be seen without staining and they can only be stained by precipitating some chemical which may add considerably to their width. They are frequently longer than the organism which possesses them and sometimes many times that length. B. symptp- matici anthracis found in the soil has a flagellum sixty times its own length. The arrangement of the flagella on the bacteria is quite constant and is used by some authors to differentiate genera. Very few of the micrococci are provided with flagella, as was indicated above, and in the bacilli and spirilla they may be arranged at the, poles singly or in brushes, or they may be arranged on the entire periphery of the cells. When bacteria are provided with a single flagellum at one pole, the arrangement is said to be monotrichous (Figs. 33 and 34). When they are arranged in brushes, the arrangement is spoken of as lophotrichous (Figs. 35 and 36) and when they are arranged on the entire periphery, the arrangement is said to be peritrichous (Fig. 37). It frequently happens that in the case of the monotrichous and lophotrichous the flagella occur at both ends of the organism. This is explained by the fact that the organism is just undergoing binary fission and that the second group is on the newly forming cell. It is worth while in this con- nection to call attention to the fact that the flagella on one end are new, while those on the other end may be thousands of generations old. THE HIGHER BACTERIA. The higher or trlchobacteria are filamentous forms. The filaments sometimes show true branching and frequently false branching. The cells are similar in form throughout the filament and are capable of independent existence, but when growing in the filament give evidence of differentia- tion. Sometimes these filaments are attached to the substratum; in other cases they are free. In the case of the sessile forms, the cells at the attached end are smaller than those at the free end. In other forms the ends may become. swollen or club-shaped. Frequently there is a difference between the cells of the different parts of the filaments indicated by the manner of reproduction. Certain cells are apparently set apart for the purpose of reproduction, and, by a process of division, form spores, or gonidia. Some of the free forms of the trlchobacteria move by undula- tive movements of the protoplasm. The exact nature of this movement BACTERIA. 55 is not understood. Many of the trick obaderia are surrounded by a mem- brane homologous to the capsule in the lower bacteria and known as a sheath. The best-known member of this group is the water-pest bacterium (Crenothrix polyspora), (Fig. 38) an iron bacterium, which has the power of oxidizing certain forms of iron, causing a deposit to accumulate in the water pipes of cities where it may cause considerable trouble. It is prob- FlG. 38. Crenothrix polyspora Cohn, Brunnenfaden. and Weiss.) (After Migula from Schmidt able also that this bacterium has had a very important part in the depo- sition of our iron ores, such as those found on the Mesaba range. Another member is the Actinomyces boms (Fig. 98) which is the cause of the common disease in cattle known as lumpy jaw. This bacterium may also infect man. Many other forms of trichobacteria are found in nature and probably play important parts in the chemical transformation of matter 56 MORPHOLOGY AND CULTURE OF MICROORGANISMS. CLASSIFICATION. The classification of bacteria was early recognized by Mueller as a matter of difficulty, since he says: "The difficulties that beset the in- vestigation of these microscopic animals are complex; the sure and defi- nite determination (of species) requires so much time, so much of acu- men of eye and judgment, so much of perseverance and patience, that there is hardly anything else so difficult." Early investigators found it difficult to decide whether bacteria are plants or animals, and nowadays we are finding it as difficult to decide upon a system of classification. A great many systems have been proposed, but many of them are untenable because those who proposed them were ignorant of or unconcerned by the rules adopted by systematists in other lines. The only system that seems worthy of continued life is that of Migula, who is a trained botanist. This system, with slight modifications, is given below. In this system, the characters which separate the genera are morphological ; while physiologi- cal characters, including cultural, are used for the differentiation of species and smaller groups. One of the rules adopted by systematists in other lines is the binomial rule. In the violation of this rule, bacteri- ologists have been great sinners, and some of the names proposed by Migula and others following his system are quite different from those by which well-known forms have been christened by their discoverers. CLASSIFICATION OF MIGULA (MODIFIED). The bacteria are phycochrome-free schizomycetous plants which divide in one two, or three planes. Reproduction takes place by vegetative multiplication (fission). Resting stages in the form of endospores are produced by many species. Motility is noted in some genera, and this is due to flagella. In Beggiatoa and Spirochseta the organs of locomotion are not definitely known. I. Order: Eubacteria(true bacteria). The cells are devoid of any nucleus (Zentralkorper) and free from sulphur and bacteriopurpurin, colorless or faintly colored. I. Suborder: Haplobacterinae (lower bacteria). I. Family: Coccaceas (ZOPF) MIG. The cells are globular when in a free state, but in the various stages of division appear somewhat elliptical. A few species in this family are motile. Cell division takes place in several directions of space. Frequently the cells remain attached to- gether, and under these conditions usually show some flattening of the cell at the point of junction with the cell next to it. Genus : Streptococcus BILLROTH. The cells are globular and do not possess any organs of locomotion. Cell division BACTERIA. 57 takes place in only one plane. Usually the cells remain united together after division, producing chains or diplococcus forms. No endospores have been noted. Genus : Micrococcus (HALLIER) COHN. The cells are globular and do not possess any organs of locomotion. Cell division takes place in two planes at right angles. If the cells remain attached together after cell division, merismopedia plates are formed. The plates give the appearance of a regular flat mass of cells. No endospores have been noted in this genus. Genus: Sarcina GOODSIR. The cells are globular and do not possess any organs of locomotion. Cell division takes place in three planes, all perpendicular to each other. Its cells remain attached after division; cube-like packets are formed. The composition of the media some- times prevents this typical cube formation. Genus : Planococcus MIGULA. The cells are globular. Cell division takes place in two planes at right angles similar to genus Micrococcus. The cells of this genus are motile, possessing one or two long flagella. No endospores are produced in this genus. Genus : Planosarcina MIGULA. The cells are globular. Cell division takes place in three planes as in Sarcina. Cells are motile, having only one flagellum on each. Cells usually remain united in twos and in tetrads and seldom form packets as Sarcina. II. Family: Bacteriaceae MIGULA. The cells are cylindrical in shape. They vary in length from short almost spherical bodies to very long rods. Cell division takes place in one direction in a plane perpen- dicular to the long axis of the cell. Some of the members of this family remain attached together, forming threads, while others separate from each other soon after fission. Genus: Bacterium EHRENBERG. The cells are cylindrical, of longer or shorter length. Threads are frequently formed. The cells do not possess any organs of locomotion. Endospores are produced in some few species, but in the majority no such formation occurs. It is possible that endospore formation occurs only under certain environmental conditions. Genus : Bacillus COHN. The cells are cylindrical, of longer or shorter length. The rods are sometimes oval in shape. Cells are motile and possess flagella which are distributed over the entire surface. Endospore formation occurs with marked regularity. The bacteria in this genus are motile only during certain periods of their life. This period varies greatly in length and occurs only in the vegetative stage. Genus : Pseudomonas MIGULA. The cells are cylindrical, of longer or shorter length. The cells are motile and possess polar flagella. These flagella may vary from one to twelve in number. The formation of endospores in this species is claimed by some. If they occur, it is ex- tremely rare. Occasionally certain species in this genus form themselves into threads or chains. III. Family : Spirillaceae MIGULA. The cells are wound in the form of a spiral or representing the portion of a turn of a spiral. In the latter case, if the cells remain attached together in the form of a 58 MORPHOLOGY AND CULTURE OF MICROORGANISMS. FIG. 39. Chamydothrix hyalina Migula. (After Migula from Schmidt and Weiss.) BACTERIA. 59 thread, a full spiral of several turns is produced. Cell division takes place in only one direction of space, and this is transverse to the long axis of the cell. Genus : Spirosoma MIGULA. The cells are rigid and bent in the form of spirals. The members of this genus are as a general rule quite large. The cells may be free or united together into small gelatinous masses. Some of the cells individually are surrounded by a gelatinous enve- lopes, while others are free. Genus: Microspira SCHRO'TER. The cells are rigid, short, and bent similar to a comma. When the cells are united together, S-shaped threads are formed. The cells are motile, possessing usually one flagellum and rarely two or three flagella. These flagella are about the same length as the cell. No endospores are formed. Some writers make no distinction between Microspira and Spirillum. The name Vibrio has also been applied by some writers to this genus. Genus : Spirillum EHRENBERG. The cells are rigid, usually long and forming long, screw-like threads, or, in some cases, only portions of a spiral turn. Cells are motile and possess a tuft of flagella at }he pole. The flagella may occur at both ends of the spiral, and they vary greatly in number. Endospore formation has been observed in some species. Genus : Spirochaeta EHRENBERG. The cells are flexible spirals, very thin and long. No flagella are present. These bacteria move by rotation similar to a screw, and also by lateral motion similar to a snake. The locomotive organs, if present, are not known. No endospores are produced. II. Suborder: Trichobacterinae (higher bacteria). Family : Chlamydobacteriaceae MIGULA. The cells are cylindrical, are united in threads, and surrounded by a sheath. Reproduction takes place by means of motile and non-motile gonidia. These gonidia arise directly from the vegetative cells and, without any resting stage, produce new threads of cells, Genus : Chlamydothrix MIGULA. The cells are cylindrical, non-motile, and arranged in unbranched threads and surrounded by a sheath of varying thickness in different species, being the same diameter at apex and base (Fig. 39). Reproduction takes place by means of gonidia, which are round and arise directly from the vegetative cell. This genus is called Leptothrix by KUTZING and Streptohrix by COHN. Genus : Crenothrix COHN. The cells are united together into filaments which are unbranched. The filaments gradually enlarge toward the free end, thus making a distinction between the apex and base. The sheath which covers the filaments is thick and often becomes infiltrated with the hydroxide of iron after being cast off in water in which there is a large amount of iron. Reproduction takes place by the formation of round gonidia which are formed in the beginning by division perpendicular to the long axis of the cell and later by divi- sion in three directions of space. Only one or possibly two species can be placed in this genus. 6o MORPHOLOGY AND CULTURE OF MICROORGANISMS. Genus : Phragmidiothrix ENGLER. The cells in the beginning form unbranched threads. Cell division takes place in three directions of space, thus forming within the sheath a mass of cells. Later these cells may burst through, multiply, and form branches after acquiring sheaths. The sheath in this genus is quite thin and can scarcely be seen. Genus: Sphaerotilus KTJTZING, 1833, (Cladothrix COHN). The cells are cylindrical and the threads are surrounded by sheaths Dichotomous branching is present, and there is no differentiation in size between the apex and base of the thread (Fig. 40) . Reproduction takes place by means of gonidia which swarm together within the cell. These gonidia burst out of the cells, attach themselves to some object, and grow into new threads. The gonidia are endowed with flagella which are attached toward the end and below the pole. II. Order: Thiobacteria (sulphur bacteria). The cells do not possess any nucleus and contain sulphur. The cells are colorless or pigmented rose, violet, or red by bacteriopurpurin. The cells are never pigmented green. I. Family: Beggiatoaceae TREVISAN. Filamentous bacteria which do not contain bacteriopur- purin. The cells contain sulphur granules. Reproduction takes place in one direction of space. Genus : Thiothrix WINOGRADSKY The cells are non-motile and the threads are attached to some object. The threads are surrounded by a delicate sheath and the cells contain sulphur granules. Gonidia are pro- duced at the end of the threads. These gonidia ear motile and finally attach themselves to some object, and, according to some authors, bend at right angles in the middle and grow into new threads. Genus : Beggiatoa TREVISAN. The threads are not surrounded by a sheath and are formed of flat cells. The cells are not attached (Fig. 41). This genus moves by means of an undula- ting membrane similar to Oscillaria. As the organism moves, it rotates on its long axis and swings its free ends. Gonidia are unknown and reproduction takes place by a division and separation of the threads. II. Family: Rhodobacteriacese (WINOGRADSKY'S classification, artificial). The cells contain bacteriopurpurin and on this account may be red, rose, or violet. Sulphur granules may also be included within the cells. FIG. 40. C I ad o- thrixdichotomaCohn. (After Fischer from Schmidt and Weiss.) FIG. 41. Beggiatoa alba. Vaucher, Trevisan. (After Winogradsky Jrom Schmidt and Weiss.) BACTERIA. 6l I. Subfamily. The cells are united into colonies. Cell division takes place in three directions of space. Genus : Thiocystis WINOGRADSKY. The colonies are small, compact, and enveloped either singly or in groups by a gelatinous cyst. The colonies are also capable of breaking up and the cells moving about. Genus : Thiocapsa WINOGRADSKY. The cells are globular in shape and spread out on a substratum in flat colonies. These colonies are surrounded by a common gelatinous secretion similar to a capsule. The cells are non-motile. Genus : Thiosarcina WINOGRADSKY. The colonies form packets similar to the genus Sarcina of the Eubacteria. The cells are non-motile. II. Subfamily Lamprocystaceae. The cells are formed into families. Cell division takes place first in three then in two directions of space. Genus : Lamprocystis SCHRO'TER. The cells in the beginning are solid, then hollow, becoming perforated like a net. They separate into small groups and become motile. III. Subfamily Thiopediaceae. The cells are united into colonies. Cell division takes place in two directions of space. Genus : Thiopedia WINOGRADSKY. The families are formed similar to tubes and are composed of cells arranged in fours and capable of motility. IV. Subfamily Amcebobacteriacese. The cells are united into colonies. Cell division takes place in one direction of space. Genus : Amcebobacter WINOGRADSKY. The cells are united into colonies, and after division in one direction of space remain attached together by threads of protoplasm. The colonies possess amoeboid motility. The cells change form by contraction and the spreading out of the proto- plasm. Genus : Thiothece WINOGRADSKY. The colonies are inclosed by a thick, gelatinous cyst. The cells are capable of moving and are very loosely surrounded by a common gelatin. Genus : Thiodictyon WINOGRADSKY. The colonies are solid, non-motile, and consist of small cells which are pressed together. V. Subfamily Chromatiacese. The cells are free and capable at all times of motility. Genus : Chromatium PERTY. The cells are moderately thick, elliptical or cylindric-elliptical in shape Genus: Rhabdochromatium WINOGRADSKY. 62 MORPHOLOGY AND CULTURE OF MICROORGANISMS. The cells are free, rod-shaped, or spindle form; they possess flagella on the poles and are motile at all times. Genus: Thiospirillum. The cells are free, continually motile, and spirally twisted. RELATIONSHIP OF BACTERIA. There has been a great deal of discussion as to whether bacteria are plants or animals. They were first described as animalcula and to the popular mind they are usually animals or "bugs." It is difficult to de- termine their exact relation philogenetically. These difficulties are so great that some scientists, as Haeckel, would create a new kingdom, call it Protista, and put in it some of the lower plants and animals which are difficult to classify, together with the bacteria. This view, however, is not a very popular one, and the attempt is usually made to trace the re- lationship of bacteria to well-known representatives of the plant and animal kingdoms. The bacteria are undoubtedly more closely related to the blue-green algae than to any other forms of life. They resemble these organisms in form, method of reproduction, and absence of definite nu- cleus. It is quite impossible to decide, furthermore, whether some forms, such as Bad. viride and Bact. chlorimtm, are blue-green algae or bacteria. On the other hand, there are some points of resemblance between the bacteria and the protozoa. Spore formation, similar to that among the bacteria, occurs among some of the protozoa. Another point of resem- blance is the possession of flagella. Some of the flagellates quite closely resemble the bacteria in many ways, and the spirochsetae, which are usu- ally believed to be bacteria, have been classed as flagellates by eminent proto-zoologists. Physiologically the bacteria are quite closely related to the fungi, and are frequently classed with them under the term Schizomycetes. ARTIFICIAL CULTIVATION OF BACTERIA. The introduction of methods of artificial cultivation marks the beginning of the science of bacteriology. These methods were developed by Pasteur and Koch and are depended upon by the bacteriologist of to-day as the foundation for most of his work. It has been the aim of investigation to discover a more general culture medium. So far it has been impossible to do this, but beef broth, made after a formula suggested by LoefHer many years ago, forms the basis of nearly all of our culture media. This beef broth, or nutrient bouillon, is made by extracting meat free from fat in water, adding a small per cent of peptone, BACTERIA. 63 correcting the chemical reaction, clarifying and sterilizing. To this broth various substances are added for special purposes; gelatin and agar, in order to solidify the media, and various sugars and other chemical substances for the purpose of determin- ing the physiological characteristics of various bacteria. One of the difficulties with the present methods of the artificial cultivation of bacteria is the inconstancy of the composition of the media, due to the fact that the extract of beef, the peptone, and other ingredients, cannot be obtained chemically pure. If it should prove possible to use synthetic substances, such as the polypeptids, it would mark a great step in advance, but it is probably quite impossible to devise a single medium upon which all bacteria will grow. Some bacteria, such as those which produce nitrification, refuse to grow on ordinary media containing organic material. The cultivation of bacteria in pure culture is dependent upon isolation, and the method of isolation suggested by Robert Koch in 1880, and known as the plate culture method, has given eminent satisfaction. This method is dependent upon the use of a liquefiable solid medium, such as gelatin or agar. CHAPTER IV. INVISIBLE MICROORGANISMS* The term "invisible microorganism" is used interchangeably with such expressions as "ultra-microscopic organism," "invisible virus" and "filterable virus" to designate a group of microorganisms which cannot be discerned with the most powerful lenses. Besides being invisible, these microorganisms will pass through the ordinary "bacteria-proof" filters and with one exception,! they have resisted all attempts at cultivation outside of the animal body. The virus of foot-and-mouth disease may be taken as a typical example. In this disease vesicles form in the mouths and on the feet of infected cattle. The virus is known to be present in the lymph which forms in these vesicles because this lymph will produce typical attacks of foot-and-mouth disease when inoculated into susceptible animals. If now this infectious lymph be diluted with water and passed through a Berkefeld filter the resulting filtrate will be found to be free from all visible microorganisms and in addition the usual culture tests will give negative results. Notwithstanding this apparent sterility, however, the filtrate will produce disease in cattle in the same manner as the unfiltered lymph. It is known that the symptoms produced by the filtrate are caused by a living organism and not by a toxin, because by successive filtrations and inoculations the disease can be transmitted through a long series of animals, thus indicating clearly that there exists in the filtered lymph a living organism which is capable of reproduction. Another proof that the virulence of the filtered lymph is caused by the presence of living corpuscular elements, and that it is not a mere solution of a toxin, is found in the failure of the virus to pass through filters of finer grain than the Berkefeld as, for example, the Kitasato filter. The more important of the diseases which may be caused by invisible microorganisms are yellow fever, infantile paralysis, hog cholera, bovine * Prepared by M. Dorset, t Bovine pleuro-pneumonia. 64 INVISIBLE MICROORGANISMS. a FIG. 42. Apparatus for fractional filtration, designed for use with Pasteur-Cham- berland or Berkefeld filters, a, glass mantle surrounding filter; b, Chamberland filter; c, paraffin joint; d and e, rubber stoppers;/, double side-arm suction flask; g, pinchcock controlling outlet from suction flask; h, outlet tube surrounded by glass shield and attached to lower end of suction flask by means of short rubber tubing; i, glass shield fused to and surrounding outlet tube as a protection against contamination when the filtrates are drawn off; j, glass inlet tube plugged with cotton, for admitting air into suction flask; k, pinchcock governing the admission of air into flask; /, vacuum gauge; m, stopcock connected with vacuum pump. (U. S. Dept. of Agriculture, Bureau of Animal Industry, Bui. 113.) 66 MORPHOLOGY AND CULTURE OF MICROORGANISMS. pleuropneumonia, cattle plague, canine distemper, swamp fever or in- fectious anaemia of horses, chicken pest, sheep pox, and horse sickness. The invisibility of this group of microorganisms may depend upon either their minute size or their peculiar structure. The most powerful microscopes will not enable us to discern with distinctness objects which are less than o.i/i in diameter. We know of bacteria which in size approach this limit quite closely (M. progrediens, 0.15^ in diameter) and there is no reason for believing that the size of organisms is limited by our ability to see them. As already stated, invisibility may also result from a peculiarity of structure, such as complete transparency and failure to stain with the reagents ordinarily used for this purpose. The ability of microorganisms to pass through niters is dependent upon a variety of factors. The size and plasticity of the organism, the fineness of the pores, and the thickness of the walls of the filter as well as the conditions under which the filtration is performed, will all influence the result. The failure of the invisible microorganisms to develop under artificial conditions is to be attributed to their strict parasitism and to our inability to imitate exactly in the laboratory the conditions which exist in the animal body. While the invisible microorganisms possess certain qualities in com- mon, in some respects they differ widely from one another. Some will pass only through the coarsest of bacteria-proof filters, while others pass readily through the densest filters, thus indicating wide differences in size or in structure. Some are very susceptible to the action of germicidal agents, whereas others are more resistant than the ordinary bacteria. Some produce disease in only one species of animal, while others show little or no limitation in this respect. The diseases produced by these microorgan- isms likewise differ markedly, some being comparatively benign and local in character, whereas others appear as the most profound septicaemias. Some are extremely contagious, while others can be transferred from one animal to another only by means of an intermediate host. In fact these invisible microorganisms seem to differ among themselves quite as widely as do those which are visible to us. The existence of an invisible microorganism is determined as follows: The infectious agent must pass through a bacteria-proof filter, which is free from imperfections as shown by tests with visible organisms of small size. Pressure exceeding one atmosphere should not be employed INVISIBLE MICROORGANISMS. 67 during filtration. The time of filtration should not exceed one hour. The filtrate should remain free from all visible bacteria as shown by microscopic examination and cultural tests. The filtrate should possess the specific disease-producing qualities of the unfiltered material. Animals infected with the filtrate should yield material which, after filtration, will in its turn possess the attributes of the original unfiltered material. CHAPTER V. PROTOZOA.* [Limited to the Study of Pathogenic Forms]. INTRODUCTION. Most of those diseases which are known to be due to an infecting agent are caused by bacteria; but some of them are caused by protozoa. The bacteria belong to the vegetable kingdom. The protozoa are minute animals; they are extremely numerous, and they are very widely distributed throughout nature. From a zoological point of view, the protozoa consti- tute an important sub-kingdom. It is sometimes diffi- cult to say whether one of these minute organisms is a plant or an animal. For this reason, the unicellular organisms are sometimes classified by themselves, as Protista, in a kingdom which belongs to neither the animal nor the vegetable kingdom; usually, however, the protozoa are placed in the animal kingdom and they are denned as organisms which have the following characteristics: "They are unicellular; they reproduce by various methods of division and, often, in addition, by conjugation; they may be solitary or united in colonies, free living or parasitic; with some exceptions, they do not possess chlorophyl." Many protozoa live in fresh water. Others live in the sea; chalk is formed from the skeletons of myriads of protozoa which once lived in the ocean. When they died, their bones fell to the bottom and formed chalk. Most of the protozoa are free-living; but others are parasitic on animals and plants. Some of the parasitic protozoa are harmless and do no injury to the hosts which support them; others produce severe diseases. Before mentioning those which cause disease (see p. 667) it * Prepared by J. L. Todd. 68 FIG. 43. Mie- scher's sac from the musculature of a hog. X30 diameters. (After Ostertag.) PROTOZOA. 6 9 will be well to consider the protozoa as a class and to study the char- racters which all have in common. STRUCTURE OF THE PROTOZOA. Most protozoa are microscopical; some of them are visible to the naked eye as individuals, or as agglomerated masses of individuals. For example, the Sarcosporidia, which occur in the muscles of mice and other animals, can easily be seen without a microscope, and the huge plasmodial masses of Amoeba, which are sometimes seen on rotting wood or in tan pits, may measure several centimeters in breadth. FIG. 44. A mceba vespertilio. (After Dqflein.) Like all living things, the protozoa are composed of protoplasm. Protoplasm is a complicated and, more or less, fluid mixture of albuminous substances. A cell may be conceived of as a tiny drop of albuminous and somewhat viscid fluid, like the white of an egg. By appropriate methods, the protoplasm of a cell may be shown to have an alveolar or foam-like structure; because the protoplasm is a mixture of two fluids, 70 MORPHOLOGY AND CULTURE OF MICROORGANISMS. one viscid and the other more labile. In such a mixture, the viscid fluid forms tiny droplets, and each of them is surrounded by a layer of the less coherent fluid (Fig. 44). The arrangement of the alveoli of the foam-like cytoplasm of a living cell is the same as the arrangement of the bubbles in a mass of foam which is artificially produced. The walls of the outer layer of alveoli, or of alveoli which surround a resistant structure within the cell, are perpendicular to the surface against which they lie. The outline of the alveoli, which are not in contact with a firm structure, is circular; an exactly similar arrangement of the alveoli may be seen in a mass of soapsuds contained in a bottle; wherever the bubbles touch an unyielding surface, their outline becomes rectangular. The protoplasm of a protozoon may be divided into two main divisions: the cytoplasm and the nucleus. The cytoplasm, as a whole, may be divided, more or less easily, into a clearer, denser, more resistant outer layer the ectoplasm; and a more fluid, granular, internal portion the endoplasm. Denser, more resistant fibers sometimes run through the cytoplasm and, like a skeleton, serve to fix the shape of the organism in which they exist. The nucleus, in its simplest form, is simply an area which is differ- entiated from the remainder of the cell by being more refractile and by being colored more deeply in specimens which have been stained by dyes. It stains deeply because it contains a substance called chro- matin. The chromatin usually occurs in granules; the granules may vary considerably hi size and they are supported upon a linin frame- work. This framework does not stain by ordinary methods and it is probably continuous with, and of the same nature as the substance which forms the alveoli of the cytoplasm. The interstices of the nucleus are filled with nuclear sap. A limiting nuclear membrane may be present, but it is not an essential part of the nucleus. The nuclear material may be all gathered together in a single mass, or it may be distributed in small granules so that, at the first glance, no nucleus seems to be present. Such a nucleus is called a distributed nucleus. FUNCTIONS OF THE PROTOZOA. Most animals are composed of a great number of cells; a protozoon consists of a single cell. In an animal which is composed of many cells, the various functions of the body are each carried out by a special type PROTOZOA. 7 1 of cell ; for example, movement is performed by the muscle cells, digestion is partially provided for by the cells of the alimentary canal, and urine is excreted by the kidney cells. A protozoon is a unicellular animal and each of these functions must be performed within the single cell of which it consists. Consequently, areas in every protozoon are differentiated so as to form portions which are each devoted to special cell functions. These portions are called organella, and by means of them all the ac- tivities of a large animal go on in an organism which consists of a single cell. The functions of the nucleus are not completely understood but it seems certain that the nucleus is a controlling center for the cell's activities. Its functions, therefore, are, roughly, two-fold; they are either concerned with the maintenance of the cell, or they are concerned with its reproduc- tion; that is, they are either somatic or sexual. Usually, both functions are subserved by a single nucleus; sometimes, however, as in the flagel- lates, they are divided between two nuclei. The activities of a protozoon may be divided into three classes: LOCOMOTION, METABOLISM* and REPRODUCTION. LOCOMOTION. The protozoa have several different methods of moving themselves about. Some of them move by the formation of pseudopodia; in this method of progression, the protoplasm flows out, in finger-like processes, from the body of the parasite and, as the proto- plasm flows into these processes, the whole organism progresses, literally, by flowing along. Some of the gregarines move about by means of a flowing of the protoplasm which always takes place in one direction; it is probable that the control of the direction of the flow in these parasites is effected by the contraction of myonemes. Myonemes are contractile fibers, which usually lie near the surface of the organism possessing them. Through their contraction, the form of the body of the parasite may be altered and, in this way, motion may be produced. Cilia are small hair- like multiple, often numerous processes, which may be placed either in definite areas or over the whole surface of a protozoon. They produce motion by waving; they usually act together and their motion has a strong simultaneous stroke in one common direction. Flagella are larger than cilia; they are whip-like processes which have a lashing movement. They are usually few in number and are often placed at the ends of the organism. REPRODUCTION. The protozoa reproduce in many different ways and *For a consideration of metabolism, see p. 82, Part II, Physiology. 7 2 MORPHOLOGY AND CULTURE OF MICROORGANISMS. several of these ways may occur in a single organism. For this reason, their reproductive power is very great; in power of repeating their like, they fall just short of the bacteria. The union of a male and a female form does not always precede multiplication; sexual connection and re- production, though now united in many animals, were originally two entirely distinct phenomena and, in the protozoa, though sexual union may be concerned with the production of new individuals, it is often especially associated with the regeneration of the protoplasm of the parasites taking part in it. VK-:V> r&alJ V; ) > "'* *ii- \ .^i^;.^:\ ^$%t$tiF$< -:-";..; -i ^^j^ga*. -^-^:,v \ FIG. 45. Stages in the division of Amoeba polypodia. (After F. E. Schulze and Lange, from Doftein.) The simplest of the methods of reproduction is simple binary division, in which the organism divides into two equal parts. A modification of this process is gemmulation, in which a small protozoon buds off from a larger parent; sometimes many buds are formed rapidly, one after the other, until the parent protozoon disappears in a swarm of daughter cells When a protozoon divides at a single division to produce a large number PROTOZOA. 73 of daughter cells simultaneously, the process is called schizogony and the young parasites are called merozoites, if a sexual fertilization has not preceded the act of division; if such a division, in which the parent organ- ism disappears, takes place after a fertilizing act, the process is called sporogony and the young parasites are sporozoites. FIG. 46. Coccidium schubergi. A-C, asexual multiplication; D-K, sexual multi- plication; Z), microgametes; E, macrogamete; F, G, fertilization; H, I, K, division and spore production. (After Schaudinn, from Dqflein.) In protozoa, as in metazoa, the essential process in fertilization is the union of two nuclei of opposite sex. Before union, these nuclei undergo a series of divisions, in which the number of the chromosomes is reduced and polar bodies are extruded. In dividing, almost all cells go through a process called mitosis. In mitosis, the chromatin of the nucleus is 74 MORPHOLOGY AND CULTURE OF MICROORGANISMS. grouped into masses which are called chromosomes. The number of chromosomes which are formed during mitosis is constant and character- istic for each species. In the reproductive areas, during the two divisions just preceding the maturity of cells which are to become ova or spermat- ozoa, the number of chromosomes is reduced to exactly one-half of the number which are formed during the division of cells outside of the re- productive areas of the same animals. The process by which the number of chromosomes is reduced is reduction, and the fragments of chromatin which are unused and which are extruded from the cell during the process are called polar bodies. Reduction and extrusion of polar bodies always precede fertilization (Fig. 46). The fertilizing processes which occur in the protozoa may be classed under three heads: Copulation, Conjugation and Self-fertilization. In copulation two whole cells unite. The cells taking part in this union are called gametes and they are male micro gametes, or female macro gametes. The cells which produce the gametes are called gametocytes. The product of the union is called a copula or zygote. If the uniting cells be equal in size the copulation is isogamous; if they be unequal, the copulation is said to be anisogamous. Anisogamous copulation, the union of two unequal cells, is most typically seen in the fertilization of a large macro- gamete by a small microgamete. Copulation is a most important fertiliz- ing process among the pathogenic protozoa. Conjugation, the second method of fertilization, only occurs among the ciliata. In it, two adult individuals are placed in apposition. The nucleus of each cell first re- duces and then divides into two halves, one male, the other female. Each organism retains its female half nucleus, while an exchange of the male half nuclei is effected. Processes of self-fertilization, such as autogamy and parthenogenesis, are included under the third heading. In autogamy the nucleus of a single cell divides into two parts. Each of these undergoes two further divisions, during which the chromosomes are re- duced and polar bodies are extruded. The two resulting, reduced, half- nuclei unite, always in the same cell, to form a new nucleus. Partheno- genesis is the development of new individuals from a female cell without a preceding fertilization; this process occurs in many protozoa, and through it may be explained some of the acute outbreaks of malaria which may occur in patients who once suffered from that disease and were thought to have been cured of it. It was said that fertilization and multiplication might be distinct PROTOZOA. 75 processes. This is evident from a consideration of the phenomena of autogamy and parthenogenesis, which have just been mentioned. Reproduction occurs in both these processes without a preceding union of two sexually differentiated cells. The DEVELOPMENTAL CYCLE of a protozoon is the history of the processes through which it may pass in the period intervening between each fertilizing act. In many of the pathogenic protozoa, an alternation of generations occurs; that is, states of being of the parasite in which an asexual method of reproduction occurs, alternate with states of being in which reproduction is effected by sexual methods. The developmental cycle is often complicated by binary division, which may occur at any point, by cyst formation, and by the intervention of a second host as a necessary factor for the existence of a part of the cycle. An alternation of generations occurs in the life cycle of the parasite which produces malaria (Fig. 125) ; this parasite is one of the most important of the path- ogenic protozoa. While it is in the body of its mammalian host, man, it multiplies by binary division and by schizogony; it multiplies, sexually, within the body of its invertebrate host, a mosquito. The host in which the adult, sexual stages of the parasite occur, in this instance the mosquito, is said to be the definitive host; hosts harboring the parasite while it is in other stages are called intermediate hosts. ENCYSTMENT. When unfavorable circumstances, such as drying, occur, many protozoa are able to surround themselves by a resistant cyst and to enter upon a resting stage of indefinite length. The cyst protects them from hurtful influences and, surrounded by it, they remain in a resting state until favorable circumstances come about once more. The power of forming resistant cysts plays an important part in the life-history of many parasitic protozoa; it is especially so with those protozoa which have become so specialized that continued existence outside of their appropriate host has become impossible for them. It is often through the formation of cysts that an infection by a protozoon is spread ; then, as in the coccidia, the presence of such a stage is abso- lutely essential in the life history of the parasite. PARASITISM. A parasite is a living being which is, at some time, directly dependent upon another, usually a stronger being. Although the word parasite is often used as though it referred only 76 MORPHOLOGY AND CULTURE OF MICROORGANISMS. to organisms belonging to the animal kingdom, parasites may be either animal or vegetable; bacteria and fungi, which live at the expense of other living beings, are parasites just as the disease-producing protozoa, and the biting insects which transmit them, are parasites. Most parasites are simple organisms, low in the scale of life. They nourish themselves without exertion, at the expense of their hosts, and, as might be expected, their unemployed organs, such as the sensory, locomotory and seizing appendages, through which food is usually ob- tained, gradually disappear; degeneration always occurs in an organism which assumes a parasitic mode of life. Organisms, such as the malarial parasite, which are wholly depen- dent for existence upon their hosts, are called obligatory parasites; those which are not, such as the infusoria usually found in the stomach of herbivorous animals, are facultative parasites. Facultative parasites often feed upon dead material provided by the host, and not upon the host itself; they are then said to be saprophytic. If a parasite is attached to a host, and neither harms nor benefits it, the parasite and host are said to be commensals. For example, the spiro- chaetes found about the teeth of many persons are usually harmless; they are commensals of their host. If the host of an obligatory parasite dies, the parasite perishes also. Consequently, it is contrary to the interest of such a parasite to destroy its host; yet parasites often do harm their hosts. The harm done by a parasite to its host is recognized by the disease caused by it. The pathogenic protozoa do harm to their hosts in three main ways: They may feed upon, and destroy cells; they may produce poisonous toxins; and their presence may do damage by me- chanically obstructing some of the functions of its host. All three of these ways are well exemplified by the action of the malarial parasite on man (p. 685). DISCUSSION OF THE CLASSIFICATION.* This grouping of the protozoa gives a general idea of the position, in zoological sequence, of the individual parasites which are spoken of in the following pages. It simply divides the Protozoa into four classes: the RHIZOPODA, the FLAGELLATA, the SPOROZOA, and the INFUSORIA; and subdivides these classes directly into genera. This is by no means a * (See page 10.) PROTOZOA. 77 complete classification of the protozoa, for there are many orders and genera which are unmentioned because they are parasitic neither in man nor In animals. The form of a protozoon may vary greatly at different stages of its development; for example, the adult trypanosome is an active organism moving by means of a flagellum, the spherical developmental form of the same parasite may have no flagellum. Consequently, the whole life history of a protozoon must be known before it can be classified with absolute certainty. The whole of the life history is known of only a few protozoa; and, though the organisms mentioned in this classification are placed in the position usually given to them, it must be understood that this classi- fication is not final, and that the discovery of new stages in the life history of some of these protozoa might make it necessary to remove them from the classes in which they have been placed; for example, before its flagellate stage was known, Herpetomonas donovani was known as Leishmania donovani, and it was classified with the sporozoa. Now it is grouped with the herpetomonads. The characteristics of the different genera and of the unimportant para- sites are very briefly mentioned in the next few paragraphs; the important parasites are treated more fully in the pages indicated by the references given, in brackets, throughout the classification. - The RHIZOPODA include the simplest forms of animal life. A rhizopod, such as an amoeba, consists of a single cell, without a protective covering, and without organs of locomotion; it moves and ingests food by means of pseudopodia. Very few of the rhizopods are parasitic; most of those which are parasitic belong to the genus Amoeba. Amoebae of different species may occur in any part of the alimentary canals of animals of many different species (p. 667). The FLAGELLATA are distinguished by possessing one or more flagella; they often have, also, a fin-like, undulating membrane. Most flagellates are free-living. Comparatively few species are parasitic; but some of these cause very serious diseases (p. 667). The SPiROCELETjE, as their name signifies, are thread-like organisms, whid seem to be coiled in a spiral. It is probable that the curves of many spirochastes lie in one plane and, consequently, that their bodies are really waved and not spiral. They often have an undulating membrane and a flagellum at either end. A Herpetomonas is an elongated organism which possesses a nucleus and a blepharoblast. The blepharoblast is 78 MORPHOLOGY AND CULTURE OF MICROORGANISMS. usually situated near the blunter end of the parasite, and from it arises a terminal flagellum. A Crithidia is an organism very much resembling a Herpetomonas, with a pear-shaped body and, sometimes, a rudimentary undulating membrane. A Trypanosoma is an elongated parasite which has a nucleus, a kinetonucleus, an undulating membrane and a flagellum. Species of Herpetomonas, Crithidia and Trypanosoma are frequently found in the intestines of insects. One species of Herpetomonas is a frequent and harmless parasite in the intestine of the house fly. The genus Trypanoplasma contains organisms which have a flagellum at either end, as well as an undulating membrane. They are parasitic in the blood of fishes. The genera Cercomonas, Monas, and Plagiomonas include small, unimportant flagellate organisms which have been found, occa- sionally, to be parasitic in man; they have been found in the urine, and in necrotic material from the lungs. A Trichomonas is a pear-shaped organism which has four flagella attached to its blunt end, and an undu- lating membrane. A species of it is sometimes found in the human bladder. Other species are common, usually harmless, parasites in the intestines of pigs, frogs and other animals. The most important species of the genus Lamblia is Lamblia intestinalis. It also is a pear-shaped organism. It has several flagella and is distinguished by possessing a depressed sucker, by which it attaches itself to the wall of the intestine of the animal in which it lives. It may cause severe diarrhoea in man, and it may produce a fatal disease of the intestines in rabbits. The SPOROZOA are protozoa which may multiply by the production of spores; they are always parasitic at some stage of their life cycle. There are very many sporozoa so, for convenience of classification, they are sub- divided into seven orders. The GregarincB have a very distinctive shape; the single cell, which composes them, is divided into two or more divisions. The first of these divisions is furnished with hooks through which the parasite attaches itself to its host. None of the gregarines are parasitic on mammals ; worms are the hosts for some of them. The Coccidia are usually parasitic within cells of their host, other than blood cells; for example, Coccidium cuniculi (p. 68 1) enters the liver cells of the rabbit, while Coccidium avium enters and destroys the cells lining the intestines of the birds which it infects (p. 681). The Hamosporidia live, for a part of their life cycle, within the red cells of the blood of their hosts. They are a very important order. The genus Plasmodium causes malaria in man (p. 682); while Proteosoma and Hamoproteus are malarial parasites PROTOZOA. 79 of birds (p. 682). The H&mogregarince are usually harmless parasites of reptiles and batrachians (frogs) ; a part of their life is passed within the red cells of their host, but they have a slowly-moving stage, somewhat resembling a gregarine, which occurs free in the blood. Hepatozoon perniciosum is the best known of a group of haemogregarine-like parasites which are parasitic, often within the white cells of the blood, in dogs, in rats, and in other rodents; so far as is known, they do not cause disease. The genus Babesia ( p. 686) includes parasites which cause important diseases in cattle, sheep, horses and dogs. Similar parasites have been found in the blood of monkeys, of dogs, of rats and other rodents. The Sarcosporidia are tube-like in shape and filled with spores. They are found within the cells of the voluntary muscles. The Haplosporidia are an important group of very small sporozoa. Some of them are parasitic in fish; one of them, Rhinosporidium kinealyi, has been found in a tumor of the nose of a native of India. The Myxosporidia (p. 688) are recognized by the peculiar form of their spores; each spore has a capsule and is furnished with one or more threads. Members of this order are parasitic in various parts of fishes and they often produce disease in their hosts. The spores of the Microsporidia (p. 688) are exceedingly small; a member of this order is the cause of pebrine (p. 688). The INFUSORIA (p. 689) are a large class. Most of them are not parasitic. They are the most highly developed of the protozoa and their bodies are more or less covered with cilia, by which they move" themselves through the liquids in which they live. In the last class, under the heading Parasites of Uncertain Position, are grouped a number of organisms which cannot be classified because so little is known of them at present. Histo plasma capsulatum (p. 689), the Chlamydozoa (p. 689) and the Ultramicroscopic "viruses (p. 64, 690) are all associated with important diseases in men and in animals. Those parasites which are important enough to require special consideration are described in the order in which they are mentioned in the classification (p. 10). Whenever it is possible to do so, a single species is taken as the type of each genus and that species, with the disease it produces, is described; if the remaining species of the genus are mentioned, they are spoken of only to indicate how they differ from the description of the type species. 8o MORPHOLOGY AND CULTURE OF MICROORGANISMS. TECHNIC. The methods employed in studying the pathogenic protozoa are very similar to those used in bacteriology. Microscopes, with the highest magnifications, are used in order that the appearance of the protozoa may be observed. The observation, with the microscope, of living specimens is a most important means of studying organisms which undergo such wide changes of form as do many of the pathogenic protozoa. Some parts of a protozoon cannot be seen in a fresh, living specimen; in order to make these structures visible, preparations must often be fixed and stained by appropriate methods; one of the methods most widely used is fixation in absolute alcohol and stain- ing by some modification of Romanowsky's stain, such as Giemsa's method. Much has been learned concerning bacteria and fungi by cultivating them on artificially-prepared culture media. Some of the protozoa can be cultivated during a part, or all, of their life cycle on similar media; but culture methods have not been so important in the study of the protozoa as they have been in bacteriology. One reason for this is, probably, that many of the parasitic protozoa live, naturally, upon certain very highly specialized cells; it is difficult to prepare a culture medium sufficiently resembling the substance of those cells to enable it to be substituted for them. Another reason is that many of the protozoa exist under widely differing conditions at different stages of their life history. Even though a culture medium might be devised suitable for one of the stages of a protozoon, it is scarcely probable that the same medium would be suitable for its growth at all stages of its development. Nevertheless, much has been learned concerning the life histories of protozoa through the employment of culture methods. Culture methods are sometimes useful in diagnosing diseases, caused by protozoa; for the multiplication of the parasites, in a suitable medium, may reveal the presence of pathogenic protozoa, when they are too few to be detected by the micro- scopical examination of the infected material from which the culture was made; for example, the flagellated stage of Leishmania furunculosa may develop in cultures of material taken from a Delhi boil in which the resting stage of the parasite cannot be found (p. 675). PART II. PHYSIOLOGY OF MICROORGANISMS* DIVISION I. NUTRITION AND METABOLISM. INTRODUCTION. PRINCIPLES OF NUTRITION AND METABOLISM. The nutrition and metabolism of microorganisms is based on the same principles that regu- late animal and plant metabolism. Only in a few instances, i.e., in the anaerobiosis and in nitrogen fixation, we have processes unparalleled in the more highly developed organisms. Since it will be necessary fre- quently to refer to plant and animal nutrition in the course of this discus- sion, these principles, therefore, are briefly discussed in the following paragraph. Green plants feed only on inorganic substances. They assimilate car- bon dioxide (CO 2 ) from the air which unites with water, nitrates, potassium, calcium, and other salts of the soil and form the body substances of the plant. The cellulose, starch, sugar, protein and all other compounds constituting the plant cells are produced from the above mentioned inorganic substances. This formation of organic compounds requires a certain amount of energy. If cellulose is burned to carbon dioxide (CO 2 ) and to water (H 2 O), a certain amount of energy is liberated in the form of heat. Consequently the same amount of energy will be needed to produce cellulose from carbon dioxide and water; for the law of the conservation of energy requires that if a certain process liberates a certain quantity of energy, the reverse process will require the same quantity of energy. Green plants get their energy from the sunlight. The radiant energy of light is transformed by the chlorophyl granules of the plant leaves into chemical energy which causes the formation of organic com- * Prepared by Otto Rahn. 6 8l 82 NUTRITION AND METABOLISM. pounds from the inorganic or mineral matter. Chlorophyl is the green coloring substance of plants, and only green plants can use the energy of sunlight for their growth. The growth of green plants is a storing of the energy of light in the form of organic matter; their metabolism is largely synthetic, i.e., building up. Plants without chlorophyl, like mush- rooms, molds, yeasts and bacteria, have to provide for their energy by some other means. Animals feed mainly on organic matter. Their body substances as protein, fat, etc., are derived from the protein, fat, cellulose, etc., of plants or of animals. Nevertheless, a certain amount of energy is required in this assimilation process, since the animal protein and fat are different from the plant protein and fat. Consequently, complex chemical changes, which require energy, are necessary for growth. Energy is also lost by radiation of heat and by locomotion. Animals, being entirely unable to use the sunlight as a source of energy, obtain their energy from the digestion of organic food. The larger part of this food is oxidized completely; this part provides for the energy. Part of the food is used for building the tissue of the body; it becomes part of the animal itself. Animal metabolism is largely analytic, i.e., destructive. More organic matter is decomposed than is formed. Often the same substance can serve both purposes: the meat eaten by a dog furnishes to it energy as well as material for growth. In other cases, certain food compounds execute only one function and not the other. The distinction between food for energy and food for growth will be of value in the interpretation of microbial metabolism. In the first part of this book, microorganisms have been divided into plants and animals, but attention has been called in various places to the fact that it is often hard to determine whether the plant characters or the animal characters prevail. This holds true not only with the morphology, but also with the physiology of microorganisms. Since none of the plants discussed in this text-book possesses chlorophyl, none of them can use light as a source of energy, therefore they depend entirely upon chemical energy obtained by the digestion of food. This means that they require organic food almost entirely, since inorganic food furnishes energy only in exceptional cases. In this respect they resemble the animals very much. The metabolism of protozoa is furnished by Todd (p. 7 1) as follows: 'The ingestion of food is accomplished in some protozoa by pseudopodia; the protozoon simply flows around and so encloses a food particle. In the INTRODUCTION. 3 same way, these protozoa flow away from waste particles which are to be excreted. Other protozoa have definite mouth areas for the ingestion of food, and definite anal areas for its excretion. Those protozoa which ingest solid food, digest it within gastric vacuoles; the food is digested in these vacuoles, as it is in many-celled animals, by the aid of enzymes and of acids. The most important of the disease-producing protozoa live within nutrient fluids, for example the blood, and they obtain their nour- A FIG. 47. A, Amoeba proteus; Na, a food particle; Cv, contractile vacuole; N, nucleus. (After Doflein.) ishment from the fluid in which they live, by osmosis; consequently, they have no definite mouth area, nor gastric vacuoles, Fig. 47. "Some of the protozoa, for example, the ciliata, possess contractile vacuoles. A contractile vacuole is a clear area which appears, grows slowly, empties itself, by a rapid contraction, of the water which has drained to it, and forms again. The water which it ejects contains the soluble waste products resulting from the metabolism of the protozoon. One function of the contractile vacuoles is, therefore, excretion; in some protozoa, they are probably also concerned with respiration. Contractile 84 NUTRITION AND METABOLISM. vacuoles are usually absent in protozoa which are parasitic within other animals." A plant character which is found in most molds and yeasts, and in some bacteria, is the assimilation of nitrates and ammonium salts, but this distinction is not at all definite, for a large number of bacteria are exceptions. It will be unnecessary, therefore, always to make a distinction between microbial plants and animals. ENERGY SUPPLY OF MICROORGANISMS. Microorganisms, like animals, require food for energy as well as food for growth, and, as with animals, one compound may often serve for both these functions. It is not always possible to state whether or not a certain compound is used for growth as well as for energy production, because the amount required for growth is always very insignificant, but the distinction exists and can be indicated by a few examples. Certain bacteria are known to live entirely on mineral matter; they use minerals exclusively for building their cell substances, resembling in this respect the green plants, and provide for the necessary energy by oxidizing mineral compounds. Two typical examples are the nitrifying organisms in soil which oxidize ammonia to nitrates. This process, ac- cording to Winogradski, is divided distinctly into two phases: the Nitrosomonas oxidizes the ammonia to nitrous acid, NH 3 + 3 O=HNO 2 +H 2 O and the Nitromonas oxidizes the nitrous acid to nitric acid, HNO 2 +O = HNO 3 These oxidation processes yield a certain amount of energy which enables the bacteria to build their cells from carbon dioxide, ammonia, and certain mineral salts. Without ammonia or without nitrous acid, respectively, these bacteria cannot grow for lack of energy; they would be like a plant without light. It is evident in this case that the food for energy is also used to some extent as food for growth. The nitrogen necessary to the bacteria is supplied by the ammonia or the nitrous acid. As an example distinguishing between the food for growth and the food for energy may be mentioned the hyposulphite bacterium studied by Nathanson. This organism oxidizes hyposulphites to sulphates and sulphur, largely following the formula Na 2 S 2 O 3 + O = Na 2 SO 4 +S Hyposulphite Sulphate Sulphur INTRODUCTION. 85 Besides, some more complex compounds, like sodium tetrathionate (Na 2 S 4 O 6 ), are formed. The bacterium builds its cells exclusively from nitrates, carbon dioxide, and mineral salts; organic food is rejected. The hyposulphite can hardly be used for the construction of the cell, and must be considered entirely a food for energy. This distinction is not confined to mineral decomposition only. The urea bacteria get their energy from the decomposition of urea into ammonium carbonate. (NH 2 ) 2 CO + 2H 2 O - (NH f ) 2 CO 3 Urea Ammonium carbonate But the urea and mineral salts are not sufficient for the development of the urea bacteria. They cannot use urea as a material for building the cells, nor can they use carbon dioxide or carbonates; they cannot grow unless a suitable material for cell construction is added. Sohngen demonstrated that a few milligrams of malic acid allow a good develop- ment of the bacteria. The malic acid was used entirely for the formation of cell substances. The energy for this formation came from the urea fermentation. This example shows clearly the different requirements for cell growth and for the energy supply. This difference exists also in the alcoholic fermentation by yeasts. Recently Lindner and Saito have shown that some yeasts ferment certain sugars, and thus can obtain energy, but they cannot use them for growth. They depend upon other organic substances for cell building material. Other sugars can be used for growth, but cannot be fermented. As a general rule, the monoses of the formula C 6 H 12 O 6 are most easily fer- mented, while the bioses with the formula C 12 H 22 O n , especially maltose, are much better adapted for growth. Generally speaking, microorganisms obtain their energy by causing chemical decompositions which may be either oxidations (nitrification, vinegar fermentation) or intramolecular changes (urea fermentation, alcoholic fermentation). Many organisms are able to cause various decompositions. Yeasts will ferment sugar to alcohol and carbon dioxide if air is completely or largely excluded, but if the yeast culture is well aerated, the larger part of the sugar is oxidized completely to carbon dioxide and water, and the alcoholic fermentation is retarded. This double action upon sugar is still more pronounced with many representa- tives of the mucor family. They oxidize in presence of air and cause 86 NUTRITION AND METABOLISM. alcoholic fermentation when submerged in the liquid. A number of bacteria can grow without sugar if oxygen is present, because they can ob- tain their energy by oxidation. In the absence of oxygen, however, they can multiply only if some fermentable material like sugar is present, because this is the only source of energy available under anaerobic conditions. The amount of energy produced by the microbial cells is generally larger than the amount required for growth. The excess energy is trans- formed to heat which causes a rise of temperature in the culture medium. The formation of heat will be discussed more in detail in one of the follow- ing paragraphs. CHAPTER I. FOOD OF MICROORGANISMS. THE COMPOSITION or THE CELL. For the study of the amounts and kinds of different food substances used by microorganisms, it will be necessary to know first the material that constitutes the cells. Naturally, the main constituent of the cell is water. MOISTURE. The amount of water in the cells of microorganisms will vary with the species as well as with the cultural conditions. The total solids of " mother-of-vinegar " are only 1.7 per cent. This should be considered as an extreme and very unusual case, owing to the spongy nature of the jelly-like cell membrane. The average water content of bacteria seems to be about 85 per cent; it varies more with yeasts and still more with higher fungi. It seems reasonable to suppose that organ- isms grown in concentrated solutions as the organisms of salted meat and the molds growing in strong sugar solutions contain more solids. Spores of molds contain much more solid matter than the mycelium; the water content in two analyses of spores amounted to about 39 and 44 per cent respectively. Bacterial spores have not been analyzed, but probably are much the same. CELL WALL. The membrane of microorganisms does not generally consist of true cellulose (C 6 H 10 O 5 ) X , though it is found in some cases. Other compounds, related to cellulose, are more common; chitin* (C 18 H 30 N 2 O 12 ), or another very similar nitrogenous compound is also found. The slime surrounding some bacteria, and the capsules, consist largely of carbohydrates, but often contain some protein. CELL CONTENTS. The main portion of the cell is the protoplasm, a mixture of protein substances, each of which has a very complex nature. Enzymes which play an important role in metabolism (page 135) ar C * Chitin when hydrolized yields glucosamine and acetic acid. C 18 H 30 N.,O 12 + 4H 2 O=2CH 2 OH-CHOH"CHOH'CHOH-CHNH-. ! CHO + 3CH- 3 37 88 NUTRITION AND METABOLISM. produced in the protoplasm and are either secreted or retained. All pro- ducts of metabolism will be found in the protoplasm of the cell in small quantities. Among other substances frequently found in microorganisms may be mentioned glycogen (C 6 H 10 O 5 ) D which can be readily detected by the brown color it gives when acted upon by iodine. Glycogen may be considered as a reserve substance stored by the organism. In the same way, fats exist in microorganisms, but are more generally found; their presence can be detected by microscopical examinations as well as by chemical tests. The amount of fat in some bacteria is surprisingly high. In the tubercle bacterium 26. to 39.29 per cent of the total solids is fat. All acid-fast bacterial cells have a very high fat content. Other bacteria also contain occasionally as much as 8 per cent fat. Yeasts seem to have a lower fat content, while in molds it has been found to vary from 0.5 to 50.5 per cent. Many other products of organic nature are found occasionally, but their importance is not determined. The minerals of the microbial cell are very essential, and like the organic materials, necessary for the life of the cell. The total ash of bacteria, yeasts, and molds, is small, about 1.5 per cent to 8 per cent of the dry cell. The important minerals which seem necessary for the con- struction of the cell are potassium, calcium, magnesium, iron, manganese, and, of the metalloids, nitrogen, phosphorus, and sulphur. Some other minerals are usually, found, but are unnecessary to the cell, as sodium and silicon. AMOUNT OF FOOD REQUIRED. The amount of food that is ordinarily decomposed by microorganisms and the amount that is absolutely necessary, differ widely. The quantity of organic and inorganic matter just sufficient to support a very weak growth is certainly very small, since a few species will multiply to some extent in ordinary distilled water. Such water, after having stood for some time, is found to contain several thousand bacteria per c.c. It may seem to the layman that in such water it would be possible to detect easily the organic and inorganic matter of the microorganisms and then it would not be considered distilled water. An estimate of the weight of bacteria demonstrates, however, that this is not the case. If we suppose the average bacterial cell to be a cylinder whose base measures one square micron and whose height is two microns (which is a high estimate) the volume of such a cell would be 1X1X2 cubic microns = o.ooi X FOOD OF MICROORGANISMS. 89 o.ooi Xo.oo2 mm. = 0.000, 000,002 cu. mm. The specific gravity of bac- teria being very nearly i, the weight of one bacterium would be 0.000,000,002 mg. ; 100,000 cells per c.c. means 100,000,000 cells per liter, which would weigh 0.2 mg. Of this total weight, at least four- fifths is water and only one-fifth is solid matter. The total solid matter in one liter of water containing 100,000 bacteria per c.c. amounts to the unmeasurable quantity of 0.04 mg. Such water will pass the tests for distilled water. How much food the bacteria in distilled water have used is impossible to say, since besides the traces of minerals in the water, they obtain some food from volatile compounds of the air like carbon monoxide (CO), carbon dioxide (CO 2 ), ammonia (NH 3 ), hy- drogen (H), and perhaps methane (CH 4 ). Under all circumstances the amount of food used is very small. On the other extreme, the maximum amount of food cannot be stated very definitely. Usually bacteria cease to cause decomposition because of the accumulation of noxious metabolic products. The ordinary bacterium from sour milk will not form more than about i per cent of lactic acid, because this is the highest acid concentration that this bacterium can endure. If this acid is neutralized, the inhibiting cause is removed, and the lactic fermentation starts anew until the maximum acidity is reached again. The amount of food decomposed depends largely upon the power of the organism to resist its own products. If the food is too concentrated, however, physical influences may interfere with the meta- bolism of the cell (p. 147). ORGANIC FOOD MATERIALS. The total weight of a large bacterial cell is estimated in the pre- ceding paragraph to be about 0.000,000,002 mg., of which only about one-fifth is dry matter. The smallest quantity that can be weighed accurately on ordinary analytical balances is o.i mg. The solid matter of 250,000,000 bacteria will amount to about o.i mg. MacNeal and associates found that the dry matter of 550,000,000 cells of B. coli weigh o.i mg. The amount of food that is used as the building material for the cell is probably larger than the weight of the cell itself, since there will be waste products, but it is of the same order of magni- tude, i.e., very small and often hardly measurable. The example of the urea fermentation (on p. 85) illustrates this point very well. 90 NUTRITION AND METABOLISM. Quite large in comparison, though, is the amount of food used to provide for the energy requirements of the cell. The quantities of protein matter decomposed in soft cheese, of sugar destroyed by alcoholic and lactic fermentations, are very large and easily determined analytically. NON-NITROGENOUS FOOD COMPOUNDS. The simplest carbon com- pound, carbon dioxide (CO 2 ), cannot possibly be used as a source of energy, because it cannot be decomposed with liberation of energy. It is used for cell construction by a few bacteria, e.g., the nitrifying and the sulphur bacteria. This must be considered an unusual occurrence, however, since nearly all other bacteria and all yeasts, molds and protozoa depend on organic matter for their cell construction. Methane (CH 4 ) can be used by one or two bacteria for growth as well as for energy, and even hydrogen gas serves as food, together with carbon dioxide, to one bacterium. As a general rule, however, hydrocarbons are not attacked by microorganisms. The compounds containing oxygen in addition to carbon and hydrogen are better adapted for microbial food. The simple alcohols can be used only by a few microorganisms, while the more com- plex alcohols, like glycerin (C 3 H 5 (OH) 3 ), mannit (C 6 H 8 (OH) 6 ), etc., are very valuable as food for most molds, yeasts and bacteria. Apparently the best nitrogen-free food compounds for microorganisms are the carbohydrates, especially the hexoses, C 6 H 12 O 6 , and the bioses, C 12 H 22 O U . They can be decomposed in many different ways, always yielding energy. They are also very valuable as material for cell construction, and as mentioned in the introduction to this chapter, the bioses are better adapted for cell construction while the monoses are more easily fermented. The insoluble carbohydrates like starch and cellulose are not as generally decomposed by microorganisms as the soluble carbohydrates, though many species have the ability to attack them. Organic acids are excellent food for the microorganisms having strong oxidizing properties, since oxidation is almost the only process of decom- position that will yield energy from acids. Some of the dibasic organic acids [succinic acid (CO 2 H' CH 2 'CH 2 -CO 2 H) and tartaric acid (CO 2 H'- CH(OH)-CH(OH)'CO 2 H)] are quite commonly used as building mate- rial ; they are often added to culture media for microbial plants. Ordinar- ily, fats are not easily attacked. They are first split into their components, glycerin and fatty acids, and the glycerin is decomposed readily while the acids are used up very slowly. Other organic compounds may be used occasionally by certain microorganisms, and probably there is no organic FOOD OF MICROORGANISMS. 9! compound that cannot be decomposed under certain conditions by certain microorganisms. Even strong poisons like formaldehyde, and insoluble compounds like paraffin, are known to serve as microbial food. NITROGENOUS FOOD COMPOUNDS. Nitrogen is an absolutely neces- sary constituent of the protoplasm, and therefore indispensable to the life of the cell. The amount of nitrogen compounds required for cell construction is necessarily very small, because of the small size of the cell. Green plants assimilate nitrogen only in the form of nitrates or ammonia; animals require proteins, or peptones, and may occasionally live on amido-acids. Nothing can be said about microorganisms in general, since some require proteins, while others can feed on ammonia, nitrates and even on free nitrogen. The few microorganisms assimilating the free nitrogen of the air are very important since they increase the nitrogen content of the soil. They must have some source of energy to form their protoplasm, and this is supplied in the soil in the form of carbohydrates, organic acids, and similar organic compounds. Unless some such compounds are available, the nitrogen-fixing bacteria cannot grow. The amount of growth and amount of nitrogen fixed depend mainly upon the amount of available food. Nitrates are more commonly used by microorganisms as a source of nitro- gen. They cannot serve as a source of energy, however, since they cannot be decomposed in any way so as to yield energy. Many molds and some bacteria can use nitrates. Ammonium salts are more readily used than nitrates, and a large number of bacteria and yeasts and almost all molds can use them in the formation of protoplasm. As a source of energy, ammonium salts can be used only by the nitrate forming bacteria which oxidize them to nitrates. The strictly organic nitrogen compounds may be used as a nitrogen source and as an energy source at the same time. This is true with the urea and with amido-acids. Many microorganisms will thrive in a solution of asparagin [(CO 2 H.CH 2 .CH(NH 2 ).CO(NH 2 )]. With the amido-acids, we leave the chemically well-known compounds and come to the very complex and chemically unknown peptones. Peptones are a very good source of nitrogen and can be used as a source of energy also by most organisms. Proteins are not quite so generally used because many of them are insoluble. Many kinds of bacteria that will grow in peptone solution do not liquefy gelatin. But a large num- ber of microorganisms have very strong proteolytic (protein-dissolving) qualities and use the protein to great advantage. Most molds and 92 NUTRITION AND METABOLISM. many bacteria belong to this class of organisms, while only a few yeasts have this ability. The absolutely insoluble compounds of protein nature, like the keratin of hair and horn, can be decomposed by only a very few organisms. Though very little is known about the nutrition of protozoa, it may be mentioned here that the saprozoic forms are not able to live on any recognized soluble food media. They require solid food (bacteria, algae, diatoms, other protozoa, etc.), and it is recorded that most of them require living organisms for food and reject dead organisms. MINERAL FOOD. The minerals needed by bacteria are used (with very few exceptions) entirely as structural food. The amount of mineral compounds is very small since they make up not more than about 8 per cent of the solid matter of bacterial cells. It is probable that the cells can exist and multiply even with smaller amounts. The necessary elements are nitro- gen, phosphorus, sulphur, chlorine, potassium, calcium, magnesium, iron and manganese. There is still some doubt about the necessity of certain other elements. Such investigations are extremely difficult because of the mere traces of chemical compounds that enter into con- sideration. These elements are assimilated usually in the form of inor- ganic salts, with the exception of phosphorus and sulphur (and, of course, nitrogen). The organic compounds of these elements may be absorbed occasionally though the mineral sulphates and phosphates are by far more commonly utilized. The use of mineral compounds for the production of energy is limited to a very few species of bacteria, while yeasts, molds, and protozoa cannot possibly utilize them. The nitrite and nitrate bacteria and the hypo- sulphite organisms have already been mentioned in connection with this. Another group consisting of a number of bacteria which are morpho- logically as well as physiologically different from the common species and which are known as the sulphur bacteria or thiobacteria (p. 60), oxidize hydrogen sulphide to sulphur, and sulphur to sulphates. The sulphur formed by this process is stored in the bacterial cells which are often found nearly filled with sulphur granules. Sulphur takes the FOOD OF MICROORGANISMS. 93 place of fat, glycogen, or other stored substances. If the source of hydro- gen sulphide ceases, the bacteria oxidize the sulphur within their cells to sulphuric acid. The second process of oxidation yields more energy than the one from hydrogen sulphide to sulphur. The so-called "iron bacteria" are another group of mineral-decomposing organisms, oxidizing ferrous salts to ferric salts. They are commonly found in running brooks and small rivers, and often develop in water pipes, sometimes forming in such large quantities as to fill them entirely. It is not certain, however, that they really obtain their energy by the oxidation of iron salts. Organisms, feeding on marsh gas, hydrogen, and carbon monoxide, have been mentioned hi the chapter on carbon supply. The very recent discovery of bacteria which can oxidize carbon as such in its elementary form may also be mentioned. OXYGEN. Oxygen is indispensable to the life of all highly developed organisms. Animals especially need it to support the oxidation that takes place con- tinuously in their cells and blood. Many animals die when the oxygen supply is exhausted. Higher plants also cannot exist very long in any atmosphere without oxygen. The more simply organized forms of life are less sensitive, and micro- organisms may grow without any free oxgyen. In the introduction to this chapter, it has been stated. that some organisms obtain their energy by decomposing organic compounds without oxidation. The fermenta- tion of urea consists of a simple addition of water. CO(NH 2 ) 2 + 2 H 2 = (NH 4 ) 2 C0 3 Ammonium Urea carbonate Alcoholic and lactic fermentations are other examples. The fermen- tative change of alcohol to acetic acid, however, is a process of oxidation. CH 3 CH 2 OH+ 2 O = CH 3 COOH+H 2 O Alcohol Acetic acid Oxygen is required for this process. Similar oxidation processes are the formation of nitrates and decomposition of thiosulphate and of 94 NUTRITION AND METABOLISM. hydrogen sulphide. Organisms which depend upon oxidizing processes for their supply of energy will not be able to grow without oxygen. This is the case with the acetic bacteria, with the nitrifying bacteria, and with many molds which are generally noted for their strong oxidizing properties. The question arises whether the organisms which provide for their energy without oxidation will need oxygen for life processes other than energy supply. The urea bacteria require no free oxygen for their fermentation, but they require it for other life functions. Certain chem- ical changes can take place within the cell of these bacteria only if oxygen is present. They require very little oxygen, but they cease to grow if it be removed completely. There are, however, certain other micro- organisms which can live in a complete absence of oxygen and there are some which die in the presence of oxygen. The organisms which require free oxygen are called aerobes; those which can live without free oxygen are called anaerobes. Among the latter are the obligate anaerobes, which develop only in the absence of free oxygen, and the facultative anaerobes which can grow either with or without free oxygen. Even the aerobic microorganisms can tolerate the absence of oxygen for a considerable length of time, perhaps for years. They will not multiply but remain dormant until they come in contact with free oxygen again. The influence of free oxygen upon the obligate anaerobic bacteria is remarkable; it does not only prevent their growth, but it kills them. Some butyric bacilli die if exposed to air for fifteen hours, while the spores of these bacilli are quite resistant. The study of these organisms is quite difficult, since it takes considerable effort to remove the last traces of oxygen from the culture media. Usually they are cultivated in an atmosphere of hydrogen; carbon dioxide and coal gas do not give as good results because these gases affect the growth of the bacteria. The best gas for the cultivation of anaerobes is nitrogen, because it is absolutely neutral, but it is difficult to obtain it free from oxygen. Anaerobic organ- isms may also be grown in a vacuum. Even the obligate anaerobic organisms can tolerate a certain amount of oxygen. We can speak of a maximum concentration of oxygen for the various organisms, and also of a minimum concentration. The minimum of oxygen for the anaerobic bacteria is nil. This is the definition of all anaerobic bacteria. The maximum concentration of oxygen varies with the species. Certain bacteria are known to be killed by very small FOOD OF MICROORGANISMS. 95 amounts of oxygen; others are less sensitive. There is enough free oxygen in the atmosphere to prevent the development of certain bacteria having purple pigment, but they multiply easily wherever there is a more limited supply of oxgyen. Their maximum of oxygen is only a little smaller than the concentration of oxygen in the atmosphere. Even the aerobic bacteria have their maximum of oxygen which is many times the amount of oxygen of the atmosphere. The following table gives the maximum concentration of oxygen for a few species. The oxygen content of the atmosphere is taken as 100. Maximum Oxygen Tolerance B. (Clost idium) butyricux, 1.35 per cent of atmospheric oxygen. B. chauvei, . 5- 2 B. cedematis maligni, 3- 2 5 Purple bacteria (Molisch), about 90 Thiosulphate bacteria (Nathansson), about 400 Pink yeast, 9 Penicillium glancum, about 1700 B. prodigiosus, 3000 These numbers mean that B. (Clostridium) butyricus cannot live unless the atmosphere is diluted to about i per cent of its original content of oxygen, either by evacuation or by other gases. B. prodigiosus is able to live even if the air is compressed thirty times, but not more. The table demonstrates also that there is no natural line between anaerobic and aerobic bacteria, and a classification founded upon oxygen supply is as arbitrary as all classifications of organisms; but like all classifica- tions, it is necessary for the designation of certain qualities of bacteria though a few species merge into the well-defined groups at both extremes. The obligate anaerobic bacteria which tolerate only a very small amount of oxygen can adapt themselves to higher oxygen concentrations by a very slow increase of the oxygen pressure. It has also been claimed that occasionally the obligate anaerobic bacteria in pure culture will grow in air. It is known that these bacteria, if cultivated in an atmosphere with small amounts of oxygen, will use up the oxygen. In what form and how the oxygen is bound cannot be stated because the quantities in question are too small to be traced in the various products of metabolism. The chemical changes instituted by anaerobic organisms are partly hydrolytic decompositions, partly intramolecular changes. Carbon g6 NUTRITION AND METABOLISM. dioxide, hydrogen, and methane are produced sometimes by the same organism at the same time and from the same food compound. This appears unusual because these gases represent the ultimate products of oxidation and of reduction. The intramolecular changes caused by anaerobic processes result mainly in a change of the oxygen atoms of the food. One side of the molecule is reduced while the other side is oxidized, as in the alcoholic fermentation, which can take place without oxygen. In the sugar molecule, each carbon atom has one oxygen atom. In the products of fermentation, carbon dioxide has two oxygen atoms to one carbon atom, and in alcohol there is only one oxygen atom for two carbon atoms. In the lactic fermentation, the oxygen, which is distrib- uted evenly in the sugar, is shifted to one side of the molecule in lactic acid H H H H H O O O O O Dextrose, H C C C C C C =O H H H H H H H H O Alcohol, HC CH Carbon dioxide, O=C=O H H H H H O O Lactic acid, H C C C = O H H These changes result in a liberation of energy which enables the organ- isms to continue their life process. Some bacteria provide for oxygen by taking it from mineral compounds. Through the agency of certain microorganisms, nitrates are reduced to nitrogen and sulphates are reduced to hydrogen sulphide by a complete removal of the oxygen from the molecule. Ca(NO 3 ) 2 -5O = CaO-(-2N H 2 S0 4 - 4 = H 2 S It seems that the opportunities for the development of obligate anaero- bic organisms in nature are not very numerous. They may develop in the animal body, in the deeper layers of soil, and at the bottom of waters. They can also develop, however, on the surface of the soil and in other places where the air has free access, provided that some aerobic organisms FOOD OF MICROORGANISMS. 97 grow there at the same time. This peculiar association of aerobic and anaerobic organisms cannot be explained simply by complete exhaustion of the oxygen in the medium by the aerobic species; the latter do not remove the oxygen completely. No other completely satisfactory explan- ation can be given. Of the facultative organisms, some prefer to grow in the presence of oxygen, like the yeasts, while others thrive better without air, as certain lactic bacteria. It has been doubted whether facultative organisms can multiply continuously without oxygen. The latest experiments with yeasts indicate that there is a limit to their anaerobic multiplication. They will develop for about 20 to 30 generations; they then need free oxygen again. With bacteria, however, the multiplication seems to have no limit in this particular. Facultative organisms thrive without air only in the presence of certain food compounds, preferably carbohydrates. If they cannot get their energy by oxidation, they depend upon anaerobic fermentations, and their ability to ferment is naturally limited to a few compounds. B. coli can grow without air only in the presence of sugars; it is customary to test for the absence of sugar in broth by inoculating with B. coli a fermentation tube which has been filled with the broth. Growth in the closed arm indicates sugar; if there is growth only in the open arm, the broth is sugar- free. Other facultative bacteria may be able to destroy protein under anaerobic conditions, though experiments show that some of them lose the power of liquefying gelatin if grown without oxygen. Some of the facul- tative bacteria can provide for their oxygen by taking it from nitrates or sulphates. It is interesting to compare the energy liberated by an aerobic and an anaerobic process. The total energy stored in an organic compound is measured by the amount of heat liberated by its complete combustion. One gram of dextrose produces 3750 calories, if burned to carbon dioxide and water. The plant producing this dextrose from carbon dioxide and water needs, therefore, 3750 calories for every gram made, which are taken from the radiant energy of the sun. The mold oxidizing i g. of dextrose completely gains in this process 3750 calories which may be used in form of chemical energy for its growth and for building up the complex compounds of cell life from small simply constructed molecules. If the mold has ceased growing, these 3750 calories will not be used but will produce a slight rise in the temperature of the nutrient medium. A yeast 7 98 NUTRITION AND METABOLISM. fermenting the dextrose to alcohol and carbon dioxide does not use the entire energy of the dextrose; there is considerable available energy left in the alcohol; carbon dioxide contains no available energy. One g. of dextrose gives about 0.48 g. of alcohol and 0.52 g. of carbon dioxide. The heat of combustion of alcohol is 7183 calories per g. or 3476 calories for 0.48 g. The heat of combustion of carbon dioxide is nil. The dextrose before fermentation represents 3750 calories, the products of fermentation contain 3476 calories; the yeast therefore gains by the fermentative process only 247 calories from i g. of dextrose. This is a very small gain, compared with that of oxidation; the ratio is 274:3750 or 1:14. This means that a yeast, in order to get the same supply of energy as an oxidizing mold, has to ferment fourteen times as much sugar as the mold oxidizes. A very good example of this is the different power of nitrogen fixation with aerobic and anaerobic bacteria. The aerobic Azotobacter fixes about 15 mg. of nitrogen for each g. of sugar, while the anaerobic B. (Clostridiutri) butyricus fixes only 2 mg. for the same amount of sugar, when this sugar is fermented to butyric and acetic acid, carbon dioxide and hydrogen. The nitrogen numbers indicate the rate of growth of aerobic and anaerobic organisms with the same amount of food. Occasionally, attention is called to the enormous destructive power of microorganisms, the proportion of food to growth being entirely different from that of animals. One reason for this difference can be plainly seen from the above discussion. The higher animals oxidize their food almost completely and consequently need only a fraction of what a fermenting organism would require. The oxygen requirements of protozoa have not been investigated until recently. It is probable that some parasitic protozoa can live and multiply without free oxygen for a considerable time. ADDITIONAL REMARKS ON MICROBIAL FOOD. PHYSIOLOGICAL GROUPS. It is customary to divide the microorgan- isms into physiological groups according to the kind of food and the metabolic products formed. This is convenient and helpful in describing certain characters though the classification and nomenclature has been accomplished as far as possible with strictly morphological characteristics, as is the custom in all classification of plants and animals. The so- FOOD OF MICROORGANISMS. 99 called "sulphur bacteria" certainly belong to one physiological group which is very plainly defined by their ability to oxidize hydrogen sulphide to sulphur and sulphuric acid. The official nomenclature distributes them, however, into several genera. The "nitrate bacteria" are another group having a very definite physiological character. In some groups the morphological and physiological characters agree very largely, e.g., in the butyric bacteria which are all spore-forming rods with a tendency to show spindle form, and in the Azotobacter group which is morpho- logically distinctly different from any other bacteria. With some other more general terms like "lactic bacterium," "putre- fying organism," "acid producer," the quality indicated is very vaguely expressed and therefore of little significance. Another feature should be mentioned in discussing the relation of microorganisms and their food, namely the fact that some organisms prefer certain foods and live exclusively on a very few chemical com- pounds, being unable to assimilate any others, while other organisms are able to feed on nearly every organic substance. The nitrifying bacteria are unable to use anything but ammonium salts. Certain pathogenic bacteria require a very special medium. The invisible organisms cannot be culti- vated on any medium except the living tissue. The fermenting yeasts can grow on protein media without sugar, though their development is meager. Some protozoa feed on many kinds of living bacteria, but cannot eat dead bacteria. Of the scavengers which can live on all kinds of food, the molds have many examples, living not only on protein, sugars, starch, cellulose, fat, but also able to exist on inferior food like alcohol, acetic or oxalic acids, with often no other nitrogen source than ammonium salt. Such omnivorous species are also found among bacteria, especially among sewage and soil bacteria. SYNTHETIC MEDIA. Recent investigations, especially by Gorham and his associates, of the physiology of microorganisms have shown that most organisms do not necessarily require media made from meat extracts, peptone and similar unknown compounds. A large number even of pathogenic bacteria which had been believed to specialize very particularly in their food requirements can be grown on synthetic media containing only compounds of well-known chemical composition, as amino-acids (asparagin, glycocoll), urea, ammonium salts of tartaric, succinic or lactic acids, dextrose, glycerin, and perhaps other organic substances, besides the necessary mineral salts. The great advantage of these media is that 100 NUTRITION AND METABOLISM. they can always be made exactly alike, while meat extracts, peptones of various manufactures, and milk, vary in composition and cannot be con- sidered as standard media. Besides, the microbiologist can follow the metabolic processes in synthetic media very easily, while it is impossible even to enumerate all the compounds contained in the ordinary nutrient gelatin, not to speak of a quantitative determination. CHAPTER II. PRODUCTS OF METABOLISM. THE CHEMICAL EQUATIONS OF FERMENTATIONS. The metabolism of all organisms is considered to be a chemical process which follows in all respects the laws of chemistry. That we are not familiar with all the changes taking place in the cell is not because we are dealing with unknown forces, but simply because we do not know all the factors involved in the process. Some of the chemical changes caused by the living cell can be imitated exactly by the chemist in a test- tube. This may be illustrated by the oxidation of alcohol to acetic acid, the decomposition of urea to ammonium carbonate and of ammonia to nitrate. Some other processes are not as fully understood and not as easily imitated. The alcoholic and acid fermentations of sugars are of such nature. There is no reason to suppose, however, that these processes are other than chemical changes. A chemical process can always be expressed by a chemical equation, consequently the various known fermentations and decompositions caused by microorganisms should be represented by chemical equations. This formulation is not always simple, because the greater number of microorganisms decompose organic substances in more than one way. Also, certain compounds may be produced in such small quantities as to escape the chemical analysis entirely, since the determination of many or- ganic compounds is a very difficult task. Again, part of the decomposed material will usually be assimilated in the growth of the cells; hence more material disappears than can be accounted for by the fermentation pro- ducts. There are several possibilities for discrepancies; accurate equa- tions can be given only for the simplest fermentations, the products of which can be analyzed more or less exactly. The best studied microbial process is the alcoholic fermentation, which is not only the classical example of fermentation, but also of great commercial importance. The simplest equation for the decomposition of dextrose into alcohol and carbon dioxide by yeast is C 6 H 12 O 6 = 2C 2 H 5 OH+ 2CO 2 180 92 88 101 IO2 NUTRITION AND METABOLISM. According to this formula, 100 parts of dextrose should give 51.11 parts of alcohol and 48.89 parts of carbon dioxide. The actual yield comes very close to these numbers, but does not reach them ; the largest amounts found were 46-47.5 per cent of carbon dioxide and 47.5-48.67 per cent of alcohol. Under the most favorable conditions, the total yield of the products of fermentation ,was only 95 per cent of the theoretical yield. Other products are formed besides the alcohol and carbon dioxide. The amount of glycerin found in fermented liquids varies very much with the conditions of fermentation; it reaches from 1.6 to 13.8 per cent of the alcohol or from 0.8 to 6.9 per cent of the fermented sugar. A small quantity of succinic acid is also formed, usually about 0.6 to 0.7 per cent of the fermented sugar. Traces of acetic acid and of lactic acid seem to be normal products of the process of fermentation. All of these com- pounds have been regarded as products resulting from the regular fermen- tation, but the latest investigations seem to indicate that glycerin and succinic acid are produced by yeast cells even in the absence of sugar. This discovery makes it probable that the glycerin and succinic acid are derived from the reserve substances of the yeast cells, such as lecithin, and are not direct products of fermentation. This accounts also for the variation of the proportion between alcohol and glycerin. Similar are the experiences with the lactic fermentation which has been studied almost as extensively as alcoholic fermentation. If it is supposed that the formation of lactic acid follows the equation C 12 H 22 11 +H 2 = 4 C 3 H 6 3 342 18 360 Lactose Lactic acid the actual yield of acid is found to be between 90 per cent and 98 per cent of the theoretical. The other 2-10 per cent are either used for cell- growth or for products which thus far have escaped chemical determina- tion. Small discrepancies will also be found in the fermentation of urea and in the nitrifying process, where small amounts of the nitrogenous material are used for the cell-growth. Another difficulty in finding the chemical equation of a microbial fermentation is the fact that this process may change with the age of the culture. In those fermentations where several gases, as carbon dioxide and hydrogen, are produced, the relative proportion of the two is not at all constant. In the butyric fermentation of dextrose by B. amylozyma, PRODUCTS OF METABOLISM. 103 Perdrix found the relation of hydrogen to carbon dioxide to be at first 65:35, later 52:48, and the relation of butyric to acetic acid 26:74, and later 85:15. Perdrix tries to account for this change by assuming three different phases of the process at various ages of the cultures, represented by the following equations: First stage: 56C 6 H 12 O 6 + 42H 2 O= n6H 2 + ii4CO 2 + 3oCH 3 COOH+ Dextrose Acetic acid 3 6CH 3 CH 2 CH,COOH. Butyric acid Second stage: 4 6C 6 H 12 O 6 + i8H 2 O= ii2H 2 +94CO 2 + i5CH 3 COOH+ 38CH 3 CH 2 CH 2 COOH. Third stage: C 6 H 12 O 6 -2H 2 +2CO 2 +CH 3 CH 2 CH 2 COOH. It does not seem very probable that the protoplasm of the butyric organism takes up 56 dextrose molecules at once and changes their molecular structures. It is possible that the hydrogen, the carbonic acid, and the organic acids are produced by three or four different processes taking place at once in the same cell independent of each other, and that by certain influences the one is favored, the other checked. But there is no proof for such a theory. In fermentations where acid is produced, it will naturally make a very great difference whether this acid is neutralized or not. All organisms are retarded by their own products, and the acid-producing bacteria often give rise to so much acid that it kills them. The neutralization of the free acid will permit them to make more acid. Oxalic acid is produced in large quantities by Aspergillus niger if calcium carbonate is present to neutralize the acid. Without calcium carbonate, only about one-sixth of the amount of acid is produced. In some instances the acidity or alkalinity' of the medium may also have a decided influence upon the nature of the products of fermentation. The proportion of acids and alcohols in butyric fermentation is said to be altered materially by the addition of calcium carbonate. Other complications occur when an organism is able to use its own products as food, as is the case with some acetic bacteria. They will at first produce considerable amounts of acetic acid and after a while they oxidize the acid completely. It becomes impossible to account for microbial activity by a chemical equation when several organic compounds are decomposed at the same time as is found to occur in some foods, as butter, cheese, ensilage and in sewage. It is also impossible to formulate 104 NUTRITION AND METABOLISM. exactly decompositions which are caused by mixed cultures. The complications become so great and the relations between different organisms are so little known that it is useless to make the attempt. PHYSIOLOGICAL VARIATIONS. The great variability of microorganisms in morphological respects has already been pointed out in Part I of this book. A similar variation and adaptation are noticed in their physiology, especially with the food sub- stances of bacteria and consequently with their metabolic products. Microorganisms change their physiological properties very readily with the environment; the new variety may keep its acquired properties for some time even if brought back to the original conditions. It is stated frequently that microorganisms tend more toward variations than the more complex organisms. It should be considered, however, that the experiences in the variations of green plants and animals are based on individuals, while in the case of microorganisms these experiences are gained almost always from millions of cells. A simple illustration is the development of bacteria in salt solutions. If a broth culture of B. coli is transferred into broth containing 8 per cent of salt, a large number of cells will die, often more than 99 per cent. The surviving bacteria begin to multiply after a certain length of time and a new variety is created which can tolerate the salt. At first, only about one out of one hundred cells had the power to tolerate salt, but, since the dying cells are not usually counted or considered at all, it is customary to say that bacteria easily adapt themselves to an 8 per cent salt solution. If only one single plant out of one hundred could be adapted to a certain high temperature, it could not be said that it adapts itself easily. This mistake is quite com- monly made with microorganisms. The best illustration for the variability of cultivated microorganisms is the enormous number of varieties of Saccharomyces cerevisia. Nearly every large brewery has a yeast type of its own which differs from others by the amount of alcohol and aromatic substances produced, by time and optimum temperature of spore-production, by the appearance of the budding yeast in the hanging drop, and also in other respects. The cul- tivated organisms are not alone in showing this tendency toward variation. The transferring of a soil or water bacterium into the ordinary laboratory media is a complete change of conditions; the different cells of the same PRODUCTS OF METABOLISM. 105 species may react differently and give several varieties. A lactic bac- terium on meat media without sugar does not thrive well in the first generations, but it gradually becomes able to grow on this medium. By this treatment, it loses gradually the power of producing acid and does not thrive as well in milk. The attenuation of pathogenic bacteria by cultivation on media, as potato, very different from the blood and muscle upon which they grow most naturally, or by growing them at low tem- perature, or above the maximum, furnishes another example. The decrease and finally the entire loss of pathogenicity is caused by a change of metabolism, by a loss of the power to produce toxin in many cases. As by certain diet the metabolism can be changed, so certain physio- logical properties of bacteria can, by proper cultivation, be increased. By the frequent transferring of an organism on gelatin, its liquefying qualities can be increased, provided it had some at the start. By continued passing of a bacterium through an animal, its virulence can be increased. Strains of bacteria which will produce a very high acidity can be bred ; this is il- lustrated by the quick-vinegar process and by the strong alcohol-produc- ing yeasts of the distillery process. It is also possible to accustom micro- organisms to certain chemicals which are antiseptic for the ordinary strains. Distillery yeast is by careful breeding acclimatized to tolerate a very high degree of acidity which would kill an ordinarily bred yeast. By continued cultivation of an organism upon a certain medium, it will be- come so acclimatized that it degenerates readily when the conditions become unfavorable. Such high-bred strains of microorganisms are used in alcoholic and lactic fermentation, in pathogenic bacteriology and in the inoculation of leguminous plants with nitrogen-fixing bacteria. PRODUCTS FROM NITROGEN-FREE COMPOUNDS. The decomposition products of nitrogen-free organic compounds will be taken up in the same order as was done with the food substances, beginning with the most complex carbohydrates. CELLULOSE is attacked by many molds, but little is known about the products. Probably they oxidize it completely to carbon dioxide and water. (C 6 H 10 O B )n+ i2nO = 6nCO 2 + 5nH 2 O Some bacteria, as B. ferrugineus (van Iterson) and a few denitrifying bacteria, can use cellulose as organic food material ; cellulose in soils is 106 NUTRITION AND METABOLISM. known to favor denitrification. The best studied decompositions of cellulose are the two anaerobic fermentations, generally distinguished as methane and hydrogen fermentation. The ' 'methane" and the "hydrogen" bacillus usually are found together; pure cultures have not been obtained as yet though the two organisms can be separated from each other. The so-called hydrogen fermentation of cellulose is caused by a thin, slender rod, producing spores at the end of the cell, some of which have drum- stick forms. The products of this destruction of cellulose are acetic and butyric acid, probably a little valeric acid, carbon dioxide, and hy- drogen. The mixture of gases contains at first more than 80 per cent of hydrogen, at a later stage it contains only 4.5 per cent hydrogen, and the remainder carbon dioxide^ The "methane" bacillus, which looks very much like the "hydrogen" bacillus, gives mainly acetic acid with a little butyric acid, while carbon dioxide and methane escape. The amount of methane is at first about 75 per cent of the total gas, but soon drops to about 30 per cent. The marsh gas in the mud of marshes, lakes, and other waters is formed by this organism. STARCH is decomposed in many different ways. It may be oxidized completely like cellulose to carbon dioxide and water. The same chem- ical equation applies to this process. Some molds and some bacteria will change the starch to various acids (lactic, acetic, oxalic, etc.) or to alcohol and carbon dioxide. In every instance, the starch is converted first into sugar, and then the sugar is fermented. The starch is not fermented directly, since it is insoluble. (The fermentations of sugar are dealt with in the next paragraph.) Dextrins are in all respects similar to starch and are also converted into soluble sugars before being fermented. Those organisms which cannot break up the starch or dextrin molecule to sugar cannot use it as food. SUGARS can be decomposed in several different ways. Some fermenta- tions have been studied much in detail, especially those of commercial importance; others are known to some extent, but no special effort has been made to determine all products quantitatively, consequently the equations of these fermentations cannot be exactly given. The alcoholic fermentation by yeasts with its by-products has been discussed so extensively in the paragraph above that there is little to be added. Among the molds, the species of Mucor are the best-known alcohol producers; nearly all mucorshave this quality and some of them, PRODUCTS OF METABOLISM. IOy imported from eastern Asia, in such a high degree that they are used for the production of industrial alcohol since they have also, unlike the yeasts, the quality of converting starch. These molds were first called "Amylomyces" though the more modern classification put them in the genus Rhizopus. Among the Aspergillacca, Aspergillus oryza is the only species which is materially concerned in the production of alcohol. It is found in the fermentation of Japanese rice-brandy, called "Sake," and has been tried in Europe as a substitute for malt to change starch into fermentable sugars. Since these molds make alcohol mainly in the absence of oxygen, when the cells are spherical (gemmae) and look like budding yeasts, it was believed for some time that yeasts were only a certain stage of development of the mucor molds. Alcohol, along with other com- pounds, is also formed by certain bacteria, though in small quantities and not as the only product; this is true in the butyric fermentation, and in gassy fermentations. Alcohols other than ethyl alcohol are produced by several organisms. Methyl alcohol (HCH 2 OH) is found to be produced by B. boocopricus from cow-dung. Butyl alcohol (CH 3 (CH 2 ) 2 CH,OH) is a common product in the butyric fermentation. B. amylozyma makes amyl alcohol [CH 3 - (CH 2 ) 3 CH 2 OH] under certain conditions, and it is probable that the fusel oil, the by-product of alcoholic fermentation in distilleries, is not formed by the yeast, but by some anaerobic organisms developing in the fermenting pulps. The use of pure cultures for the production of fusel oil, especially amyl alcohol, has been suggested. Besides alcohol, organic acids are very commonly produced from sugar by many bacteria, yeasts and molds. The acid fermentations have wide practical application, and much attention has been paid to their study. If, however, our knowledge, especially of the quantitative relations between food and products, is limited, this is largely due to the great variability of the organisms and the difficulty of analysis. The best known, because the simplest, fermentation, is the pure lactic fermentation which has already been discussed on page 102; it is very nearly represented by the equation C 6 H 12 O 6 = 2CH 3 CH(OH)COOH Dextrose Lactic acid The bacteria which cause this fermentation are called true lactic bacteria. They are the main acid producers in milk. Other acid producers form gas besides lactic acid or other acids or alcohol. In IO8 NUTRITION AND METABOLISM. the group of gas-producing lactics, B. coli and Bad. aerogenes are the main representatives. The fermentation of dextrose by B. coll is very nearly described by the equation 2 C 6 H 12 O 6 + H 2 O = 2 C 3 H 6 O 3 + CH 3 COOH+ C 2 H 5 OH+ 2 CO 2 + 2 H 2 Dextrose Lactic acid Acetic acid Alcohol A certain group of bacteria, including the Bad. aerogenes, the Strept. pneumonia, and B. typhosus, cause fermentations which are very similar to the one above. The products depend not only upon the species but also upon the fermented sugar. Grimbert found that B. coli makes acetic acid from all fermentable sugars, but lactic acid only from dextrose, while with all the other sugars, succinic acid is formed instead of lactic acid. B. typhosus gives no succinic acid, but always lactic and acetic acid, often also butyric acid. The mechanism of these fermentations is apparently not as simple as that of the alcoholic and the true lactic fermen- tation. The greatest difficulty for the physiologist is the change of products during the fermentation; at first one, later another product predominates, consequently an attempt to give a certain definite equation of the fermentation is frustrated. It is more convenient merely to enumer- ate all products than to give an equation which may hold true only with a certain stage of growth of a single variety under one set of conditions, without giving any guarantee that other strains under different conditions will give even approximately the same kinds and quantities of products. In this group of gas- and acid-forming bacteria, we find a number of organisms of practical importance. They are the organisms of the fermentation of sauerkraut, dill pickles, brine pickles, ensilage. There are further B. coli and a number of pathogenic bacteria, B. typhosus, and the varieties of the Strept. pneumonia. The standard products are acetic acid and alcohol, besides carbon dioxide and hydrogen; lactic acid is usually, succinic acid often, produced. The products depend upon the fermented sugar, the amount of oxygen present, temperature, the presence of neutralizing agents and possibly some unknown factors. Acetic acid is, besides the lactic acid, the most common acid formed by microorganisms. Formic acid (HCOOH) is produced by a very few bacteria (B. ethaceticus, page 1 1 1) and occasionally by some molds, while acetic acid is a very common product of fermentation. In the decomposition of sugars, it is never the only product; other acids, gases or alcohols are formed besides acetic acid. Pure acetic acid is produced PRODUCTS OF METABOLISM. only in acetic fermentations, not from sugar, but from alcohol, by a very simple process of oxidation. CH 3 CH 2 OH+ 2 0=CH 3 COOH+H 2 O Alcohol Acetic acid If there is not plenty of air present, the oxidation may not become complete and small amounts of acetaldehyde may form. CH 3 CH 2 OH+O=CH 3 COH+H 2 O Alcohol Aldehyde Some acetic bacteria can destroy acetic acid by oxidizing it completely CH 3 COOH+ 4 O = 2CO 2 + 2H 2 O Molds frequently form acetic acid from sugar or starch; the peculiar acid taste of moldy fruit preserves is due partly to this acid. Another product of fermentation of sugars which has been mentioned already in various places, is butyric acid (CH 3 CH 2 CH 2 COOH). It has the very pungent odor of rancid butter. Butyric acid is formed not only from carbohydrates, but also from butter fat and from proteins. The production from cellulose has been discussed at the beginning of this chapter. The difficulty of giving an equation for butyric fermentation of dextrose has been pointed out in the chapter on chemical equations. Butyric acid is, like acetic acid, not the only product of fermentation. It is always accompanied by other acids and alcohols. The butyric bacteria are distinguished and named according to the predominating products of fermentation. They were known as B. (Clostridium) buty- ricus, B. butylicus, B. lactobutyricus and B. lactopropylbutyricus. Recent investigations of Bredemann have made it probable, however, that most of these bacteria are only varieties of the same species. The amounts of the different acids and alcohols formed by one strain vary with varying con- ditions so much that a dominance of the one or the other product cannot be used for diagnostic purposes. Butyric acid is also produced from lactic acid and from glycerin. These fermentations have a theoretical interest, because they represent a synthesis by bacteria; glycerin or lactic acid, with three carbon atoms, are changed to butyric acid with four carbon atoms. In the decomposition of sugars by bacteria, mainly monobasic acids are formed; lactic, acetic and butyric acids are predominant, though occasionally succinic acid is also found. Yeasts change the sugar to alcohol and carbon dioxide almost exclusively. The mycoderma 110 NUTRITION AND METABOLISM. species are able to produce a little acid. The most characteristic quality of molds is their great oxidizing power which enables them to use many different kinds of organic substances for food. Besides this oxidizing quality, they have also the power of causing acid fermentation or alco- holic fermentation. The acids produced by molds are mostly di- and tribasic. Besides the acetic acid, oxalic and citric acids are produced by molds. Oxalic acid is formed, especially by the Aspergillacea, in large quantities, if some alkali, like calcium carbonate, is present to neutralize the free acid. Aspergillus niger, the typical oxalic-acid mold, is supposed to oxidize dextrose according to the following equation: C 6 H 12 6 + 9 = 3(COOH) 2 + 3 H 2 The yield of oxalic acid is, however, only one-half of what could be expected from the above equation, because of the very pronounced oxidizing qualities of this mold; it will oxidize part of the dextrose, or of the acid, completely to carbon dioxide and water. If the acid is not neutralized, the mold will finally oxidize all the oxalic acid to carbon dioxide and water. Citric acid (CH 2 (COOH)COH(COOH)CH 2 COOH) is formed by many molds. Some of them produce it in such quantities as to render possible the manufacture of citric acid from glucose by the use of molds. The process can be expressed by the following equation: C 6 H 12 6 + 3 0= C 6 H 8 7 + 2 H 2 The mold uses, however, about twice as much sugar as would be expected from this formula, because of its strong oxidizing power. This discussion involving the products of the decomposition of sugars is far from complete, but aims to touch the most common fermentations. ALCOHOLS. Besides the carbohydrates, another group of food sub- stances has to be mentioned which is closely related to the sugars, namely the higher alcohols. The two main representatives are mannit (CH 2 OH.- CHOH.CHOH.CHOH.CHOH.CH 2 OH) and glycerin (CH 2 OH.CHOH.- CH 2 OH). Mannit differs from the simplest sugars only by having two additional hydrogen atoms which indicates that the aldehyde or ketone group of the sugar is changed into an alcohol group in the mannit. The products of mannit fermentation are very similar to those of sugar fer- mentations. Different organisms give different products among which alcohol and acetic acid prevail. The Strept. pneumonia decomposes it in the following way: PRODUCTS OF METABOLISM. Ill 6C 6 H 14 O 6 + H 2 O = 9C 2 H 5 OH+ 4 CH 3 COOH+ ioCO 2 + 8H 2 Mannit Alcohol Acetic acid while the B. ethaceticus makes formic acid instead of hydrogen. 14 O 6 + H 2 O = 5C 2 H 5 OH+CH 3 COOH+CO 2 +5HCOOH Glycerin is decomposed in many ways. It may be oxidized com- pletely or it is fermented into the same products which are derived from sugars. The butyric fermentation of glycerin has already been mentioned. There are also some compounds formed from glycerin which are not found in carbohydrate decomposition. These are the products of partial oxidation, glyceric aldehyde and glyceric acid CH 2 OH CH 2 OH CH 2 OH I I I CHOH CHOH CHOH i r i CH 2 OH COH COOH Glycerin Aldehyde Acid The only monovalent alcohol of general occurrence, ethyl alcohol, undergoes only one method of decomposition, namely that of oxidation. This may be incomplete resulting in aldehyde or acetic acid (p. 109) or if the combustion is total, in carbon dioxide and water. The acetic-acid formation is the result of the acetic bacteria. Total combustion is characteristic of molds and Mycodermce. ORGANIC ACIDS are valuable food for many microorganisms, in the free form as well as in the form of salts. On acid liquids like fruit juices and jellies, sour milk, sauerkraut, pickle brine, a flora of acidophile organ- isms develops, among which the molds of the Oidium type and the Myco- dermce predominate, while bacteria are found in insignificant numbers. These acidophile organisms destroy organic acids, especially lactic and acetic acid, by total combustion. The oxidation process for lactic acid would be For all other acids, the equation is very similar. Some acids are fermented by bacteria by processes more or less similar to sugar fermen- tations. There are so many different possibilities that only a few exam- ples can be mentioned. B. tartar icus decomposes tartaric acid to acetic and succinic acid. The same organism can also ferment succinic acid, 112 NUTRITION AND METABOLISM. the products of which have not yet been analyzed. The calcium salt of lactic acid gives with B. bulylicus butyric acid with a little acetic acid. FATS are esters of glycerin with fatty acids. They can be hydrolyzed, like all esters, and thus give free acids and glycerin. The following equation shows the hydrolyzation (saponification) of tristearin: (C 18 H 35 O 2 ) CH 2 + H 2 O C 18 H 35 O 2 H CH 2 OH I I (C 18 H 35 2 ) - CH + H 2 = C 18 H 35 2 H+ CHOH I I (C 18 H 35 2 )-CH 2 +H 2 C 18 H 35 2 H CH 2 OH Tristearin Stearic acid Glycerin Only a few microogranisms are able to decompose fat to glycerin and fatty acids, and these appear to be the only organisms which can destroy fat. This saponification is the only known method of fat decomposition. After this first step is accomplished, the glycerin and acids are open to decomposition by the methods described above, either by complete combustion or otherwise. The most significant change, perhaps, in the decomposition of fat is a production of free acids from the neutral fat molecule. There are still a few compounds occurring in nature which should be considered, inasmuch as they are products of bacterial activity, and are more or less constantly forming. The most important ones are methane and hydrogen. Both of these gases are used by certain bacteria in a very unusual metabolism as a source of energy. B. methanicus (or B. oligocarbophilus) oxidizes methane completely. This organism requires no other organic food. It is retarded or inhibited by organic substances since it takes the carbon only hi form of methane or carbon dioxide and the nitrogen only in mineral form as nitrate or ammonia. In its life requirements, it resembles very much the nitrate and sulphur bacteria. This bacillus is also able to oxidize carbon monoxide to dioxide and to get all the necessary food and energy supply: in this way. The "hydrogen" bacterium is called B. pantothropus by its discoverer because it is able to live on ordinary laboratory media as well. If no other substance is available, it will oxidize hydrogen. This oxidation does not occur directly, as would be expected, following the equation PRODUCTS OF METABOLISM. 113 but it requires the presence of carbon dioxide, which is reduced by the hydrogen to formaldehyde. CO 2 + 4 H=HCOH+H 2 O. The formaldehyde is then used by this bacillus as a food and oxidized. The presence of traces of formaldehyde in the cultures can easily be proved. PRODUCTS FROM NITROGENOUS COMPOUNDS. The products resulting from microbial action upon nitrogenous compounds are largely unknown or poorly defined. They are very num- erous and many of them are of such complex nature that they cannot be determined accurately; even the testing for their presence or absence is often very difficult. It is therefore utterly impossible and quite unneces- sary to mention even all the known products and the equations of their formation. The aim is to give a thorough understanding of the gradual degradation of the protein molecules to smaller molecules of less com- plex nature, until finally crystallizing bodies are reached. These are well-defined chemical bodies and the further decompositions can be followed more exactly by chemical methods. As in the preceding chapter, the most complex compounds will be discussed first. The keratin bodies of hair, epidermis, horn, are absolutely insoluble and only very few organisms can attack them. The products have been studied but very little and do not seem to differ essentially from the cleavage products of protein bodies. PROTEIN BODIES are as numerous as plants and animals. Each species of organism seems to have its particular protein which differs from that of other species. With the more highly developed organisms, there are several distinctly different proteins found in the same individual in different parts of the body. The chemical structure of the protein mole- cule is not known. The constituents, carbon, oxygen, hydrogen, nitrogen, and sometimes sulphur and phosphorus can be determined in their relative amounts without, however, furnishing any knowledge of the structure of the molecule. The molecular weight of proteins is estimated to be at least 10,000, while the weight of the very large molecule of sac- charose is only 342. The protein molecule can be broken up into smaller 8 114 NUTRITION AND METABOLISM. molecules. This is generally believed to be a hydrolytic process similar to the decomposition of starch to maltose, or of saccharose into dextrose and levulose. The first products of protein decomposition do not differ essentially from the original protein, but they can be hydrolyzed again and again, until finally products of crystalline nature are found which are well- defined chemical bodies. Among the very first products of protein degradation it is usually impossible to determine single compounds, but several groups of compounds may be separated by certain precipitants, as acetic acid, ammonium sulphate, zinc sulphate, copper sulphate, tannic acid and others. In order to determine the degree of protein degradation, e.g., in the analysis of cheese, it is customary to determine the nitrogen of compounds precipitated by these various reagents, and state it in per- centage of the total nitrogen. Thus the terms "water-soluble nitrogen," "acid-soluble nitrogen" and others originated, meaning the nitrogen of the compounds soluble hi water or in acid respectively. Some of these groups of degradation products have been named and defined more accurately, of which the albumoses and peptones are the most common and best described compounds. Their chemical nature and structure is, however, just as little known as that of the protein bodies. The amino-acids are the first well-known compounds of protein de- composition. They are organic acids, in which a hydrogen atom is substituted by a NH 2 radical. Some of them are simple compounds, as the amino acetic acid NH 2 CH 2 COOH and also the amino-capronic acid, usually called leucin, (CH 3 ) 2 CH CH 2 CH(NH 2 ) CO OH. Others are of a more complex nature, such as the tyrosin or hydroxy-phenyl- amino-propionic acid, C 6 H 4 (OH) CH 2 CH (NH 2 ) COOH, and the tryptophan or indol-amino-propionic acid, C 8 H 6 N CH 2 CH(NH 2 ) COOH. Of other nitrogenous products which are not amino-acids, a few are of striking significance. The very disagreeable odor of putrefying proteins and of excreta is due to indol (C 8 H 7 N) and methyl-indol or skatol (C 8 H 6 N CH 3 ). Indol gives a rose color with nitrites in acid solution, and this convenient reagent is used in the identification of bacteria. Another group are the amins, hydrocarbons in which one or several hydrogen atoms are replaced by an NH 2 radical. The simplest amins are the methyl-amins, of which the tri-methylamin (CH 3 ) 3 N is produced by several bacteria. The fishy odor of the brine of salted herring is largely due to this compound. In this group belong also a large number of the so-called ptomains. PRODUCTS OF METABOLISM. 1 15 The ptomains (p. 417) are alkaloid-like bodies of basic character and of more or less well-known structure. Some of them are notorious for being very strong poisons, while others are quite harmless. These bodies are usually called ptomains because they were first discovered in putrefy- ing corpses. The best-known compounds of this character are the putrescin or tetra-methylen diamin [NH 2 (CH 2 ) 4 NH 2 ] and the cadaverin or penta-methylen diamin [NH 2 (CH 2 ) 5 NH 2 ], which can scarcely be considered poisonous. The methyl-guanidin / HN=C< X NHCH 3 may be mentioned as an example of a very poisonous ptomain. Another poisonous ptomain is the neurin CH 2 =CH N(CH 3 ) 3 OH which has been found frequently as a product of putrefaction. All the products of protein degradation mentioned so far may be formed in the absence of oxygen. The decomposition of protein to amino-acids is partly hydrolytic, and probably it consists also of intra- molecular changes comparable to the alcoholic and lactic fermentations. None of the processes mentioned so far requires oxygen. Even the amino-acids can be hydrolyzed further under anaerobic conditions, form- ing ammonia and hydroxy-acids. HOH+NH 2 CH 2 COOH=NH 3 +HOCH 2 COOH Amino-acetic acid Hydroxy-acetic acid In this way, ammonia is formed quite commonly from amino-acids. In the products of protein degradation mentioned above only those compounds have been considered which contain nitrogen. It is quite evident, however, that in the cleavage of the large and complex protein molecules, certain pieces of the broken molecule will contain no nitrogen. An example of how such nitrogen-free compounds might be formed is given in the hydrolysis of amino-acetic acid to hydroxy- acetic acid. Many organic acids, like acetic, butyric, capronic, benzoic and phenylacetic acids are quite generally found among the products of putrefaction. Alcohols too, especially benzene derivatives like phenol and cresol, are not unusual at all. Gas is often formed in putrefaction, especially carbon dioxide and hydrogen; occasionally these gases are mixed with traces of nitrogen and methane. Carbon dioxide is formed to some extent by the hydrolysis of organic acids, as the following example shows: Il6 NUTRITION AND METABOLISM. Hydroxy-phenyl-acetic acid Cresol The formation of hydrogen, methane, and nitrogen is not as easily explained and probably means a more complicated change of the molecule than a simple hydrolysis. Many protein compounds contain, besides the organic elements, carbon, oxygen, hydrogen and nitrogen, larger or smaller amounts of phosphorus and sulphur. The phosphorus compounds may be changed to phosphine (PH 3 ), which is a gas of a strong disagreeable garlic odor. Generally, however, the phosphorus of protein after its degradation is found as phosphoric acid (H 3 PO 4 ). Very little is known about the phosphorus of organic compounds and the changes it may undergo in the putrefaction process. The sulphur of proteins is commonly changed to hydrogen sulphide (H 2 S). This may be the result of a hydrolytic cleavage or of a reducing process. Some microorganisms are able to form mercaptan (CH 3 SH), a compound of very foul penetrating odor. The production of all these compounds may take place under strictly anaerobic conditions. Hydrolysis and intramolecular rearrangements of the atoms within the molecule suffice to account for these changes. The products of this anaerobic decomposition are mainly ammonia, amins, amino-acids, alcohols (phenol), acids (acetic, butyric, capronic), hydroxy-acids, phosphoric acid, hydrogen sulphide. Many micro- biologists emphasize the distinction between the putrefaction as an anaerobic process, and the decay as an aerobic process. The anaerobic putrefaction produces offensive odors caused by indol, skatol, butyric and capronic acids, amins, phenol, and hydrogen sulphide, while the aerobic decay does not show such products. This distinction between putrefaction and decay is an artificial one, however, and cannot always be carried through. Facultative anaerobes will decompose proteins in different ways with air and without, and in nature both processes usually take place at once. It has been mentioned in the chapter on oxygen requirements that many obligate anaerobes can grow exposed to the air if at the same time some aerobic organisms develop in the same medium. This is the case in most of the decompositions occurring in soil, in the dead leaves of the forests, in manure piles, in spoiling foods. If oxygen has free admittance to the decomposing protein, the above PRODUCTS OF METABOLISM. IIJ mentioned products will be readily oxidized to simpler compounds and finally to carbon dioxide, water, ammonia; the ammonia may be oxidized further to nitrous or nitric acid, as has been mentioned already in several chapters. The final oxidation of the carbon compounds is the complete combustion, accomplished at once, or in successive steps by different organisms. Hydrogen sulphide is oxidized to sulphur or sulphuric acid. Thus we obtain as the final products of protein degradation carbon dioxide, water, ammonia, nitrates, nitrogen, hydrogen, hydrogen sulphide, sulphuric acid, phosphoric acid. The protein is completely mineralized. UREA, URIC ACID, HIPPURIC ACID are the products of protein digestion in the animal body. Urea is a normal product in the urine of many animals, especially the carnivora, while hippuric acid is produced mainly by herbivora and uric acid is one of the main constituents in the excreta of birds and snakes. The fermentation of urea to ammonium carbonate has been discussed extensively in the chapter on metabolism, page 85. It is a simple hydrolysis. CO(NH 2 ) 2 + 2 H 2 O = CO 3 (NH 4 ) 2 . Only one group of bacteria, the urea bacteria, can perform this change, a few molds are also said to cause this fermentation. Hippuric acid is of much more complex nature, benzoyl-amino-acetic acid. It is probably split up by bacteria into benzole acid and amino-acetic acid C 6 H 5 CO. NH CH 2 COOH +HOH=C 6 H 5 COOH+NH 2 CH 2 COOH Hippuric acid Benzoic acid Amino-acetic acid Uric acid, also a complex organic body, can be oxidized through the agency of bacteria by several processes which yield ammonium carbonate and carbon dioxide. Often urea is an intermediate product forming in the following manner: Uric acid Urea The decomposition of these three compounds takes place continuously in manure piles and in sewage. The final result is, as with proteins, a complete mineralization. PRODUCTS FROM MINERAL COMPOUNDS. Minerals are used by microorganisms for cell construction almost exclusively; consequently, they do not leave the living cell like fermenta- tion products. But a few organisms can actually decompose mineral Il8 NUTRITION AND METABOLISM. matter and when this takes place mineral products are secreted. Two main processes can be distinguished, oxidation and reduction. OXIDATIONS are the result of the organisms seeking a supply of energy. Several oxidations of minerals have been indicated previously, as the oxidation of ammonia to nitrites, of nitrites to nitrates, of hyposulphites to sulphates, of hydrogen sulphide to sulphur and of sulphur to sulphuric acid, of ferrous salts to ferric salts. All these microbial changes are simple processes and can be followed by chemical analyses much more easily than organic fermentations. The organisms which cause these changes do not thrive in organic substances and for this reason pure cultures can be obtained only with difficulty. Their activity is of great impor- tance in soil fertility. REDUCTIONS of minerals by organisms have not been discussed. They, too, are of great significance. As a typical example, nitrates may be reduced to nitrites, to ammonia, to nitrogen gas, and, rarely, to nitro- gen oxides. The reduction may be performed either by the direct removal of oxygen, or by the formation of hydrogen. The reduction of nitrates to nitrites can be written in the following three ways: KNO 3 - O = KNO 2 KNO 3 = KNO 2 +O KNO 3 + 2H= KNO 2 +H 2 O . The result in all three cases is the same. Many bacteria can reduce nitrates to nitrites or to ammonia. A few can reduce them to nitrogen. These "true denitrifiers" are found in soil and in old manure. Their reducing process is as follows: Ca(NO 3 ) 2 - 50= CaO+ 2N. Nitrates are reduced through the efforts of the organism to secure a supply of oxygen. The denitrifying bacteria have strong oxidizing prop- erties; they take oxygen from all sources possible. If cultures of denitri- fying bacteria are well aerated, as in soils with a proper moisture content, they scarcely attack the nitrates, while they will reduce them in ordinary liquid cultures so fast that the escaping nitrogen gas forms a froth on top of the nitrate solution. Denitrifying bacteria need the oxygen to oxidize organic matter. They cannot live without organic food. It has been stated previously that the oxidation of ammonia to nitrates liberates energy, consequently the reduction of nitrates must absorb energy, and PRODUCTS OF METABOLISM. 119 nitrates can be reduced by the denitrifying bacteria only if they can use the oxygen to advantage; that is, if they can obtain by the oxidation of organic bodies more energy than they expend in the reduction of the nitrates. The same rule holds true with other reductions. Sulphates are reduced in a very similar way to hydrogen sulphide H 2 SO 4 - 4 O = H 2 S. Tap-water, containing calcium sulphate, often forms hydrogen sulphide if shut off from the air for some time. While only a few bacteria reduce sulphates, many reduce sulphites or sulphur to hydrogen sulphide. The potassium and sodium salts of selenic and telluric acid (H 2 SeO 4 and H 2 TeO 4 ) are reduced by certain organisms and not by others. The reduction results in a colored precipitate; this reaction has been suggested as a diagnostic means to distinguish different species. The reduction of arsenious oxide to arsin (AsH 3 ) is used as a very delicate test for arsenic; it is applied in. the detection of arsenical poisoning. The contents of the stomach are sterilized and inoculated with Penicillium brevicaule (p. 22), the "arsenic mold." This will re- duce most arsenious compounds to arsin (As H 3 ) or to diethyl arsin, As H(C 2 H 5 ) 2 , both of which are easily recognized by their very pro- nounced garlic odor. UNKNOWN PRODUCTS OF PHYSIOLOGICAL SIGNIFICANCE. Among the products of microbial action, there are certain substances which must be mentioned because of their importance, though their quantity is insignificant compared with the ordinary products of fermen- tation. These substances can be divided into four groups: pigments, aromatic compounds, enzymes, and toxins. The chemical structure of pigments and of many aromatic substances is scarcely known; and as far as enzymes and toxins are concerned, it is not even determined whether or not they are of protein nature. The last two groups are known only by their actions, while the pigments are very conspicuous and cannot possibly be overlooked. PIGMENTS have naturally attracted the attention of microbiologists ever since pure cultures were known, and many investigators have tried to explain the nature and the meaning of pigments. All experiments concerning the purpose of pigment-formation by microorganisms have been 120 NUTRITION AND METABOLISM. without results. It is not known that the pigment is of any material advantage to bacteria; for it is possible to cultivate colorless strains of pigment bacteria which grow apparently as well as the orginal pigmented culture. Again, pigments cannot take the place of the chlorophyl in plants except perhaps the bacteriopurpurin of the purple bacteria. It does not even protect the cells against intense light, because the pigmented organisms are not more resistant than the corresponding colorless "sports." The only exception are the colored spores of the molds, especially Penicillium and Aspergillus, which are very resistant to light, while the spores of Oidium are killed just as easily as the mycelium. Pigments cannot be considered as reserve substances, since many pig- ments are excreted and remain outside the colorless cells. Pigment production may be incidental. It is possible that the waste products of certain organisms happen to be colored. After Beyerinck, the chromogenic bacteria may be divided into three classes: 1. Chromophorous bacteria, in which the pigment is placed in the cell and has a certain biological significance analogous to the chlorophyl of higher plants. In this division belong the green bacteria discovered by Van Tieghem and Engelmann and the red sulphur bacteria or purple bacteria. 2. Chromoparous or true pigment-forming bacteria, which set free the pigment as a useless excretion, either as a color-body or as a leuco-body which becomes colored through the action of atmospheric oxygen. The individuals themselves are colorless and may under certain conditions cease to form pigments. To this class belong B. prodigiosus, Ps. Syn- cyanea, Ps. pyocyanea, and others. 3. Parachrome bacteria, which form the pigment as an excretory pro- duct but retain it within their bodies, as B. janthinus and B. violaceus When the pigment is soluble in water, as those produced by Ps. pyo- cyanea and the fluorescent bacteria, it diffuses through the medium. When the pigment is not soluble, it either lies within the cell wall or be- tween the individuals. This classification furnishes some details concerning the methods of pigment production, which depends upon the presence of certain media; according to Sullivan, sometimes certain mineral salts, sometimes sugar will stimulate chromogenesis. The same is true with molds. Very brilliant colors appear with certain species of molds if grown on cellu- PRODUCTS OF METABOLISM. 121 lose or on fat, while on gelatin the pigment is not produced. The tem- perature is an important factor. A large number of chromogens produce no pigment when grown in the incubator. It is possible to obtain non- pigmentation with many species by propagating them through many generations at high temperatures. Oxygen also is necessary for the chromogenesis of many bacteria. Some need a short exposure to day- light in order to produce their pigment, while cultures grown in absolute darkness may remain colorless. Strong sunlight, however, will check pigment production in the same degree as do antiseptics and other harmful influences. The chemical nature of microbial pigments is little known. They are distinguished according to the solubility in various liquids, water, alcohol, FIG. 48. Bacteriopurpurin, from a Rhodospirillum, crystallized from a chloroform solution. (After Molisch.) ether, chloroform, benzol, and other solvents, and according to the change of color caused by acid and alkali (Fig. 48) . A group of carotin bodies, named because of their similarity to the pigment of carrots, the prodigiosin bodies, named after B. prodigiosus, the fluorescent pigments and per- haps a few other groups are distinguished, but their chemical nature is rather vague as yet. The absorption of distinct lines of the spectrum by solutions of these pigments is claimed to be a very reliable means of distinguishing the pigments of different species. AROMATIC SUBSTANCES constitute another group of metabolic prod- ucts. The chemical analysis accomplishes more with these compounds than with pigments, since they are frequently well-known compounds. 122 NUTRITION AND METABOLISM. The main difficulty arising in their identification is in the very minute quantities of the products available. Some substances with strong, mostly very disagreeable odors have already been mentioned: indol, skatol, hydrogen sulphide, mercaptan, the amins and ammonia, butyric acid, and some of the higher alcohols. There remain to be mentioned cer- tain oils and esters giving rise largely to pleasant aromas. The formation of aromatic oils has been established although their nature is entirely unknown. The same is true with the esters. The substance causing the fishy flavor in butter is volatile with steam and is neither of an alkaline nor acid nature. The strong odor of freshly plowed earth is caused by an Actinomyces; the odor can be traced to a very volatile oil the nature of which has not been determined. The aroma of fermented liquids- wines, beers, and many others is partly due to compounds constituting the fermenting material, and partly to the fermenting agent. Some yeasts are known to produce fruit-esters, as succinic-acid-ethylester and the corresponding esters of malic and other acids. Besides, some glucosides may be split and traces of hydrocyanic acid and benzoic acid may be liberated. The change of flavor with the aging of wines is probably more a chemical than a biochemical change. ENZYMES AND TOXINS. Among the most interesting and least understood products of microbial action are the enzymes and the toxins. These two groups are related in many respects. The enzymes will be discussed extensively in the following chapter and toxins are treated more extensively in Pt. Ill, Div. VII, Chap. II. Toxins and enzymes are formed by the cells in such small quantities that they would never have been discovered by ordinary chemical means were it not for the unusual effects which they produce, the enzymes acting upon food substances, and the toxins acting physiologically upon organisms. Toxins and enzymes are chemically unknown. It is assumed that they are chemical bodies, but even this has not been proved. A pure toxin has never been obtained and we have no criterion for its purity. The presence of a toxin is recognized only by an animal test, and in this way the com- parative concentration can be determined approximately. Such standard- ization of toxin solutions is only comparative, however, and gives no clue as to the actual amount of toxin present. Not all animals are sensitive to all toxins. It is quite possible that all bacteria produce compounds with chemical qualities similar to toxins, and only a few of them happen to react upon men or animals. PRODUCTS OF METABOLISM. 123 Toxins are not always the product of microbial action. Vegetable toxins or phytotoxins are known, among which the ricin of the castor- oil bean is perhaps the most studied representative. The best-known zootoxin is the rattlesnake poison. These non-microbial compounds have the same quality as the microbial toxins they are extremely poison- ous. Toxins are largely responsible for contagious diseases as diphtheria, tetanus and perhaps many others. If a culture of these organisms is filtered through a porcelain filter which removes all bacterial cells, the filtrate injected into an animal will cause the disease with all its accompa- nying symptoms though there are no microorganisms introduced into the animal body. If the filtrate is heated, however, no effect will take place after the injection, because heat destroys the toxin. The amount of toxin that will kill an animal is extremely small; 0.000005 mg. of the purest tetanus toxin will kill a mouse, 0.0007 m - f r i cm w i^ kill a rabbit, less than 0.23 mg. of tetanus toxin will kill an adult man. The body of an animal or man forms an anti-body against the toxin which neutralizes its poisonous action. Anti-bodies are also formed against enzymes injected into an animal. Toxins are very sensitive to heat. A short exposure to temperatures between 80 and 100 will inactivate them. They are also very sensitive to light. While some toxins are secreted, others are retained within the cells of microorganisms, and never leave them until the cells die or disin- tegrate. Ptomains, which are also metabolic products of microorganisms and sometimes cause poisoning, differ from the toxins in their resistance to heat and light (p. 115). Ptomains differ in no way essentially from ordinary organic compounds; the animal or human body produces no anti-ptomains to counteract their poisonous effects. There is no chemical relation whatever between toxins and ptomains, and the physiological effects are also quite different, though they both cause poisoning. Toxins are not essential products of the metabolism of pathogens. Strains of pathogenic bacteria can be bred which do not produce toxins as chromogens can be bred without pigment, or lactic bacteria which do not produce acid. The strains which lose their pathogenicity grow better on artificial media, but are less able to produce disease in the animal. They may regain the power of producing toxin if passed through the body of the animal. The real object of toxin production by micro- organisms is not known; the microorganisms derive no apparent benefit 124 NUTRITION AND METABOLISM. from the death of the animal ; the toxin may be an incidental waste product like the pigment. ROTATION OF ELEMENTS IN NATURE. All organic matter on earth is undergoing continuous change. Or- ganisms grow and decay. The same carbon and nitrogen atoms which constitute the organic world of to-day constituted it thousands of years ago. The amount of carbon, nitrogen, hydrogen and of all other elements of life on earth is limited, and the same atoms will be used for the future generations of life that constitute the present. There are two mam fea- tures in organic life, construction (anabolism) and destruction (katabolism) . Construction is mainly the task of green plants, enabled by the chlorophyl to use the energy of sunlight in building up organic substances from minerals, water and carbon dioxide. Destruction is caused mainly by animals and other organisms which have to break down organic matter in order to exist. These two factors keep the atoms of the organic world in perpetual rotation. In this circulation of the elements it is necessary that all compounds of organic nature be decomposed finally to a form available for plant food. If this were not the case, the indestructible compound would sooner or later accumulate in such enormous quantities that the elements constituting this body would be removed entirely from general circulation. Let us suppose, as an illustration, that for some unknown reason, all urea bacteria on earth would die. Urea could be decomposed no more, and the plants, unable to use urea as a source of nitrogen in place of nitrates, would get but little benefit out of stable manure. All urea would pass gradually undecomposed into rivers, lakes, and finally into the ocean where it would accumulate continuously. The enormous quantities of nitrogen taken out of circulation would cause a decreasing growth of plants, and life would soon cease because of lack of nitrogen. For this reason all products of living organisms must be further broken up by some other organisms, and we find that the destructive work is to a large extent the task of microorganisms. Many products of organic life cannot be broken down by organisms other than bacteria, and therefore bacteria are absolutely necessary for the circulation of the elements and for life on earth. Bacteria and green plants are an absolute necessity for the maintenance of life, the one breaking down, the other building up, PRODUCTS OF METABOLISM. I2 5 one dependent upon the products of the other; animals, however, could be excluded from the circle without interfering with a continuation of life on earth. CARBON CYCLE. Carbon is the main element in organic nature, and so dominant that the term carbon compounds is practically identical with organic compounds. Carbon is contained in the carbon dioxide of the air which is usually considered a mineral or inorganic compound. It is absorbed in this condition by the green plants, and is changed by the chlorophyl gran- anisms Carbondioxicle Carbohydrates fat, Protein FIG. 49. Carbon cycle. ules of the leaves to organic compounds of various types, either to car- bohydrates (cellulose, starch, sugars) or to fats, or to protein substances, occasionally to organic acids or other compounds. The plants will either die and decay, or will be eaten by animals. In the first case, the decay will be caused exclusively by microorganisms; if the plants are eaten, they will be digested; part may be used to build up the animal body or stored as reserve substances, largely fat and protein. If the animal dies, a decomposition process will take place, which breaks down the organic compounds to simpler products and finally the carbon will be completely oxidized to carbon dioxide. Even the marsh-gas which might be liberated in this process will find organisms that oxidize it to 126 NUTRITION AND METABOLISM. carbon dioxide and water. Every product will find an organism to break it up further until it is completely disorganized and the carbon atoms can start the same circulation anew. Undoubtedly as long as organic life has existed on earth, microorganisms have been present, in order to render the dead organic matter again available for plant and animal life. Figure 49 gives a schematic illustration of the carbon cycle; the microbial activity is marked by heavy lines. NITROGEN CYCLE. Nitrogen shows the same continuous change as carbon. Plants take up nitrogen in mineral form usually as nitrates. Dead Organisms //2t rates Pro tein FIG. 50. Nitrogen cycle. The plants change this mineral nitrogen to the most complex bodies, proteins, where it is combined with the other elements of organic nature. The plants may be eaten by animals; part of the protein is then digested to urea or hippuric or uric acid, which in turn are readily decomposed by microorganisms to ammonia (Fig. 50). Part of the protein will be stored in the growing animals, and if the animal dies, the body will decay or putrefy, and the nitrogenous compounds of that body will pass through the various stages of decomposition to the final product, am- monia. Ammonia is then oxidized to nitrites and nitrates, when the nit- rogen cycle is completed. There is, however, one discrepancy in this cycle. It has been men- tioned already that some organisms are able to reduce nitrates to nitrogen gas. This is one of the "leaks" in the rotation of elements which would PRODUCTS OF METABOLISM. 127 be disastrous to organic life on earth if there were no means to compensate for the loss of nitrogen in circulation. Imagine what would happen if there were no such compensation! Part of the nitrate in the soil is destroyed, the nitrogen gas escapes into the air and is as indifferent as the nitrogen of the atmosphere, lost to organic life forever. More nitrate would be produced from decaying organic matter and would be destroyed. After a certain time, this continuous loss of nitrogen would become quite noticeable in the growth of plants; there would be a scarcity of nitrogen in soil, since part of it is lost continuously. Finally, the plants would cease to grow because the nitrogen in the soil would be exhausted. Sulnidt. n U rgan/3/nj FIG. 51. Sulphur cycle. The compensation for this destruction of available nitrogen is found in the nitrogen-fixing bacteria, which either living in symbiosis with leguminous plants or growing independently in the soil, have the power to use the atmospheric nitrogen for the formation of their own protoplasm. Thus, organic nitrogen is produced from nitrogen gas and the constancy of organic life is guaranteed. SULPHUR CYCLE. Little more can be said about sulphur, since the rotation is quite similar to that of nitrogen. Plants will take sulphur usually in the form of 'sulphates and make protein compounds containing a certain amount of sulphur (Fig. 51). These bodies are either di- gested by higher animals or broken down by putrefaction to the final 128 NUTRITION AND METABOLISM. product, hydrogen sulphide, which is oxidized by the sulphur bacteria first to sulphur, then later to sulphates. PHOSPHORUS CYCLE. The cycle of phosphorus has not been worked out completely, but from the discussion in the last pages, it is plainly seen that a simple cycle very much like the ones above must exist. It is probably much simpler because phosphorus does not enter as easily into organic compounds as nitrogen. PHYSICAL PRODUCTS or METABOLISM. PRODUCTION or HEAT. It has long been known that fermentation produces heat. The rise of temperature is usually not very great. In lactic fermentation it amounts to about i, in alcoholic fermentation to 2 or 3, but in certain processes the heat liberated is considerable, as in the fermentation of manure, of ensilage, of vinegar, and in others. The cause of heat formation is quite evident from the discussion on page 98. Organisms decompose organic matter which means a liber- ation of energy. Part of this energy is used for the continuation of life- processes; the rest, usually the larger part, is not employed and appears in the form of heat. The amount of heat produced can be measured directly with the thermometer if great care is taken that no heat is lost by radiation or by evaporation of water. The best known fermentation of this character is the vinegar fermen- tation. In the quick-vinegar process (page 456) the temperature rises sometimes as high as 10 to 15 above the temperature of the room and the vinegar manufacturer uses the heat produced by the bacteria to keep the generators at the optimum temperature. If the process is not con- trolled carefully, the vinegar bacteria are likely to produce sufficient heat to kill themselves. The heat produced in the fermentation of manure, especially horse manure, is used in the hot-beds to cultivate and force young plants. In the manure pile, great heat production is not desirable because high temperatures will volatilize the ammonia; the tight packing of manure which keeps out the oxygen will prevent too strong bacterial action. The highest temperature in silos which has been recorded is about 70, but the best silage is secured by keeping the temperature below 50. Ensilage fermentation is not thoroughly understood, however, and no accurate statements can be made as to the cause of the increase in temperature. PRODUCTS OF METABOLISM. I2Q Sometimes the temperature in silos does not exceed 35. The curing of hay is usually accompanied by a rise of temperature. For some time it was believed that the spontaneous combustion of hay was mainly due to microorganisms, but it has been shown recently that even sterile hay will show a rise of temperature under certain conditions. This does not exclude the formation of heat in hay by microorganisms under other circumstances. The heating of tobacco, of green or moist grain or corn is probably not of bacterial origin, but due to chemical oxidation or to the respiration of the living plant tissue. PRODUCTION OF LIGHT. The light-producing or photogenic organ- isms are quite numerous and occur more frequently than is generally believed. The phosphorescence of decaying tree stumps and leaves in the woods and of meat and fish in the cellar are well-known phenomena. The phosphorescence of wood and leaves is generally caused by Hypho- mycetes; certain mushrooms have this quality in a very high degree. The light of meat and fish is usually generated by bacteria, of which at least twenty-six species have been described. Many experiments have been carried on in order to discover the nature and origin of the light, but, so far, few results have been obtained. The phosphorescence is due to an oxidation process; all photogenic organisms cease to generate light when the oxygen is removed. As soon as they come in contact with oxygen again, they produce light immediately, and this sudden flashing is used occasionally by physiologists as a very delicate test for oxygen. The light appears to be produced always within the cell; no cell product has ever been found to give rise to light outside the cell. It is possible that a chemical compound is formed in the cell which gener- ates light when in contact with oxygen. The life processes of the photogenic microorganisms are not necessarily connected with the formation of light. Photogenic bacteria are known to lose the power of light production as the chromogenic bacteria may lose the power of pigment production. Phosphorescence has, like pig- mentation also, no bearing upon the development of the cell, and the light- giving compounds may be regarded as incidental waste products. Cer- tain chemical bodies stimulate light production, while others favor the growth only. One of the most important factors in the production of light is sodium chloride. CHAPTER III. MECHANISM OF METABOLISM. GENERAL THEORY OF METABOLISM. ANABOLISM AND KATABOLISM.- The study of the physiological mechanism of the cell is the most interesting and most difficult problem of biological research, for it tries to discover the secret of life processes. The physiological mechanism of the cell consists of three parts generally distinguished one from the other, being interdependent upon each other Fermentation, intra- and extra-cellular, katabolism, the dissociation of cell substances, and anabolism, the assimilation of food in the synthetic processes of the cell. The katabolic processes have been studied suc- cessfully for a long time, and our knowledge of the digestion of organic and inorganic substances has a definite chemical basis. Digestive pro- cesses can be accomplished in vitro, but the cell is required to furnish the digestive agent which, after being removed from the cell, may be treated as a definite chemical compound. The katabolism, consisting of many destructive chemical processes, some of which are well-defined and some wholly unknown, represents the degeneration of the cell. The study of the anabolic or synthetic processes is to a large extent speculation. Very meager is the positive knowledge of the chemical changes involved, and only the very simplest of these reactions can be duplicated in vitro. The problems of digestion have attracted the attention of scientists long before microorganisms were known, and the knowledge of the digest- ive processes of man and animals have helped the microbiologist in many ways. Again, many results of microbiological research which could be obtained only with single-celled organisms are employed now to great advantage in general physiology. INTRA- AND EXTRA-CELLULAR FERMENTATION. DECOMPOSITION OF INSOLUBLE FOOD. It has been stated before that many microorganisms feed upon cellulose, starch, fat, gelatin, keratin and other insoluble compounds. It has also been previously stated that microorganisms, with the exception of some protozoa, depend upon 130 MECHANISM OF METABOLISM. 131 soluble food since they have no means of incorporating insoluble com- pounds into their protoplasm. The protoplasm, however, must be con- sidered the center of metabolism, and the digestion of food and the forma- tion of energy must take place in the protoplasm if the cell is to profit by it. Since the food cannot diffuse into the cell, and the protoplasm does not diffuse out, the food must be dissolved. This is accomplished by the cell itself, which secretes certain agents having peculiar qualities. These agents, the so-called enzymes, act upon the insoluble foods, changing them into soluble compounds which then can diffuse into the cell where they are digested or fermented. The final digestion or fermentation of the food must take place within the cell. Energy production outside the cell serves the same purpose as a stove outside the house. The dissolution of insoluble compounds by cell secretions must be considered a preparatory process which has no direct relation to intra-cellular food digestion or fermentation. Enzymes are not produced by microbial cells exclusively. All living cells produce enzymes. They were known before the science of microbiology had been established. In fact, microbial activity was considered for a long time as an enzymic chemical process. Enzymes in the animal and plant body may serve largely the purpose of metabolic changes. In the animal body, many enzymes help to dissolve the insoluble food which cannot pass from the alimentary canal into the body except by diffusion through the mucous membrane. There is diastase in the saliva which acts upon starch, there is pepsin in the stomach and trypsin in the intestine, both dissolving pro- tein bodies; there is ereptase for the peptones, lipase for the fat, invertase for the saccharose, and many other enzymes. The object of all these enzymes is apparently to prepare the food for passing through the mem- brane into the protoplasm of the cells, where the final changes which liberate energy take place. The same processes occur with micro- organisms but in a more simple manner. Surrounded by a liquid medium, they secrete specific substances (enzymes) ; these dissolve certain insoluble foods which then diffuse through the cell wall to be decomposed further. The food-preparing processes are all supposed to be simple hydrolytic processes. For some of these changes the chemical equations are well known. The hydrolyzation of starch to maltose by means of diastase is represented by the equation 2 (C 6 H 10 5 ) n +nH 2 = 132 NUTRITION AND METABOLISM. The splitting up of a fat molecule into glycerin and fatty acid is also a well-known process C 3 H 5 (C 18 H 35 2 ) 3 +3H 2 = C 3 H 5 (OH) 3 + 3 C 18 H 36 2 Tristearin Glycerin Stearic acid The proteolysis is not so well known and the general supposition that the first stages of protein degradation are hydrolytic is largely based upon analogies. Some of these enzymes which are secreted by the microbial cells act upon soluble compounds. Invertase decomposes saccharose into dextrose and levulose: C 12 H 22 11 + H 2 = C 6 H 12 6 +C 6 H 12 6 Other disaccharides are hydrolyzed in the same way by other enzymes; glucosides are decomposed by emulsin; soluble proteins are changed to peptones. It is not necessary that the enzymes act upon the soluble com- pounds outside the cell since these compounds can diffuse into the cell; these enzymes are found only occasionally within the cell. It may be said, however, that the smaller molecules of the products of ^nzymic action diffuse more readily than the larger molecules of the original food compound. PROPERTIES OF ENZYMES. These secretions of cells are treated in a group by themselves because they differ distinctly in many respects from any other chemical substance. Probably the most notable differ- ence may be discovered in the fact that their action does not follow the law of mass action which supposes that all substances reacting upon each other diminish in quantity. This is not the case with enzymes. Rennet will coagulate many hundred times its weight of casein, and still the whey will contain rennet. Considering that part of the rennet is physically absorbed by the coagulum, the amount of rennet is found to be the same as before, though it has changed a comparatively enormous quantity of casein. The same is true with other enzymes. The enzyme is not destroyed by acting upon other substances. This exceptional quality furnishes a reason for treating enzymes as a separate group or apart from other chemical substances. But there are still other qualities which distinctly separate them from the well-known chemical bodies, and show at the same time their relation to proteins and toxins (page 122). One of these is their sensibility to such outside influences as will destroy life. Enzymes are inactivated by exposure to temperatures above 50 to 80, and can, like coagulated albumin, by no means be brought back to MECHANISM OF METABOLISM. 133 their orginal state. They have, like organisms, a maximum, optimum and minimum temperature of activity, and if heated above the maximum they will be destroyed. In this respect they resemble albumin since the maximum temperature for enzymes is very near the coagulating tempera- ture of albumin. It is believed from this resemblance that enzymes are of an albuminous nature. Another similarity is the fact that both enzymes and albumins are precipitated by concentrated salt solutions. Enzymes can further be inactivated by poisons. The same sub- stances which kill living cells, like formaldehyde, hydrocyanic acid, mercuric chloride, phenol, will also inactivate enzymes, though usually stronger solutions are required for the destruction of the enzyme than for killing the cell. It is the same with heat; a higher temperature is generally required to destroy the enzyme than to kill the cell which se- creted it. Light will also affect enzymes considerably. The great simi- larity of enzymes and microorganisms in these respects, the similarity of their reactions and the extreme minuteness of the bacteria render it explicable why the chemists of eighty years ago could not deter- mine the difference between microorganisms and enzymes. With the toxins, the enzymes have in common the great sensibility to heat, light, and chemicals. Both of these groups are resistant to drying to a limited extent. So far as body reactions are concerned these two groups seem to belong to one physiological group of compounds. When toxins are injected, the body responds by the production of anti- toxins which inactivate the toxin. In the same way the body responds to enzymes by the production of anti-enzymes which prevent the action of the enzymes. It may be mentioned that against protein compounds, precipitins are produced by the body which precipitate only that protein which was injected. This "specific" action is also true with toxins and enzymes. The anti-body will inactivate only the specific kind of toxin or enzyme that was injected. What an enzyme really is cannot be defined. An enzyme is known only by its reactions. Many chemists have tried to prepare pure enzymes by continuously dissolving and precipitating, by dialyzing and other means, but there are two great difficulties existing; there is no test for the purity of enzymes, and they lose in activity if treated with chemicals. The more they are freed from the protein bodies which always accompany them, the more sensitive they are to injurious influences. The purest enzymes that have been obtained do not give the reactions of protein 134 NUTRITION AND METABOLISM. substances. Mineral salts seem essential for their action, because con- tinued dialyzing weakens the activity which can be restored only by adding salts. MECHANISM OF FERMENTATION. It has been demonstrated in the above paragraph that food is prepared for digestion or fermentation by enzymes. The final decomposition, the process which yields the energy for cell life, must take place within the cell. The investigations of recent years have demonstrated that these processes also are caused by enzymes. It has been proved beyond doubt that in the alcoholic, lactic, acetic and urea fermentations the fermentation process may continue after the death of the fermenting cells. In the case of alcoholic fermenta- tion, the fermenting agent has been separated from the lacerated cells and has been filtered through porcelain filters without losing its ability to act. This proves the enzyme-nature of the fermenting agent which after once being formed, remains and acts independent of the cell. These enzymes are called zymases. They remain within the cell as long as it is alive. They are much more sensitive to injurious influences than the above mentioned food-preparing enzymes. Much skill and patience was required to demonstrate their independence of the living cell. After these enzymes were found in microorganisms, similar enzymes were discovered in the cells of higher plants and animals. Many of the bio- chemical changes taking place in the final dissociation of food within the cell are now known to be the result of enzymic action; heretofore these reactions were believed to be a part of the life-processes, inseparable from the living cell. Even some of the oxidations and many reducing processes have been recognized as caused by enzymes, and it is quite possible that the whole process of intracellular food decomposition is accomplished entirely by means of enzymes. CLASSIFICATION OF ENZYMES. Since the chemical nature of enzymes and of their action is largely unknown, they can be classified only according to the compounds they act upon. It is possible, however, to distinguish between the following four groups: Hydrolyzing, zymatic, oxidizing, reducing enzymes. This definition is not quite exact, since the urea fermenting enzyme is also a hydrolyzing enzyme, and the acetic fermentation is caused by an oxidiz- ing enzyme. The distinction between endo-enzymes (infra-cellular) and MECHANISM OF METABOLISM. 135 exo-enzymes (secreted) is not exact, either, since invertase and lactase are retained in the cells of some organisms and secreted by others. The following classification is used in the further discussions: I. Hydrolytic Enzymes. 1. of carbohydrates: cellulase (cytase), diastase (ptyalin, amylase), invertase, lactase, maltase. 2. of fats: lipase (steapsin). 3. of proteins: a. proteolytic (proteases): pepsin (peptase), trypsin (tryptase), erepsin (ereptase). b. coagulating: thrombase, rennet (chymosin). II. Zymases. 1. of carbohydrates: alcoholase, lactacidase. 2. of other nitrogen -free bodies: vinegar-oxidase. 3. of proteins: endo-tryptase, autolytic enzymes, amidase, urease. III. Oxidizing Enzymes. Vinegar-oxidase, tyrosinase. IV. Reducing Enzymes. Katalase, reductases of nitrates, sulphur, sulphites, telluric salts, methy- lene blue, litmus. Several names have been given to some of the enzymes; these are found in parentheses in the above classification. The general action of enzymes being explained in the preceding pages, it remains to describe more in detail the different enzymes of microbial origin. HYDROLYTIC ENZYMES. ENZYMES OF CARBOHYDRATES. Enzymes which decompose carbo- hydrates are very commonly found in nature, because carbohydrates constitute a very extensive and common group of organic matter. By far the largest part of the dry plant consists of cellulose, starch and sugar. To decompose them, enzymes are necessary. The chemical reaction of these enzymes is hydrolytic; in other words, the larger molecule is broken into smaller ones by the simple addition of water. Thus, the cellulose-destroying enzyme, called cellulase or cytase, decomposes the cellulose into soluble sugars after the following formula: C 6 H 10 5 +H 2 0=C 6 H 12 6 or, considering that the cellulose molecule is really many times C 6 H 10 O 5 , the formula will be more accurately written (C 6 H 10 5 ) n +nH,0 = 136 NUTRITION AND METABOLISM. which indicates at the same time that one cellulose, molecule gives many sugar molecules. Cellulase is an enzyme which is quite difficult to obtain. Though it must be produced by all the cellulose destroying molds and bacteria, experiments have failed in some instances to prove its presence. It is found in some wood destroying fungi and in some of the bacteria causing the rot of vegetables. The organisms of certain plant diseases force their way into the cell by dissolving the cellulose membrane by an enzyme, while certain molds are able to puncture the cell wall mechanically. Diastase, or amylase, is the starch-dissolving enzyme which is one of the most common enzymes in nature. It is found in all green plants, and it forms during the sprouting of starchy seeds. Many molds and a few bacteria produce this enzyme, while yeasts generally cannot decompose starch for lack of diastase. Starch has the same formula as cellulose, and it is broken up into soluble sugars in the same way. Much attention has been paid to this process by the chemists, and it is found that the process is a gradual one, giving first dextrins, and finally maltose (C^H^On). The hydrolysis of starch expressed in chemical symbols may be presented as follows: 2 (C 6 H 10 5 ) n + nH 2 = nC 12 H 22 n Starch Maltose The disaccharides or double sugars, having the chemical formula C 12 H 22 O U are broken up into single sugars, monosaccharides, by the following process: C 12 H 22 U + H 2 0= C 6 H 12 6 + C 6 H 12 6 The two molecules of C 6 H 12 O 6 are different with different sugars. If the disaccharide is saccharose, the two monosaccharide molecules are dextrose and levulose. Lactose will yield dextrose and galactose, and maltose will give two molecules of dextrose. For each of these sugars, there is a special enzyme which can hydrolyze only its particular sugar and none of the others; like a key, made for one lock, it will not open another lock. Maltase will split only maltose molecules, not lactose, while the lactase cannot attack the maltose. Invertase (or sucrase) will decompose nothing but saccharose. This decomposition of the complex sugars into the simple sugars is necessary because only sugars of the type C 6 H 12 O 8 can be fermented directly by the fermenting enzyme in the cell, be it an alcoholic or lactic or gassy fermentation. This explains why beer yeast MECHANISM OF METABOLISM. 137 cannot ferment lactose; it produces no lactase, and therefore cannot attack the lactose molecules; they would be easily attacked, if besides the yeast, some lactase were added. Certain lactic bacteria cannot ferment saccharose, because they do not form invertase. Invertase is, like diastase, a very common enzyme in green plants. It is also produced by the larger number of molds and yeasts, and also of bacteria. Maltase is not quite so common, and lactase is limited to a few species of microorganisms. A few organisms are known which do not secrete these enzymes but retain them within the cell. This is especi- ally true of lactase, but is also known, in a few instances, of invertase. The enzyme can be obtained from the broken cells. Such enzymes are called endo-enzymes. The decomposition of carbohydrates has been followed from the most complex representatives to the simplest ones, the monosaccharides. If these are decomposed further, the resulting product is no longer a carbohy- drate. The simplest sugars are decomposed by zymases, inside the mi- crobial cell, into compounds which are generally called fermentation products; these may result from alcoholic, lactic, butyric fermentations or some other. Emulsin is an enzyme which is able to hydrolyze glucosides. Gluco- sides occurring in plants are complex bodies which contain a sugar-radical. Emulsin splits glucosides liberating the sugar, usually dextrose. The typical example for emulsin action is the hydrolysis of amygdalin to hydrocyanic acid, benzaldehyde and dextrose. C 20 H 27 O n N+2H 2 O=C 6 H 5 COH+2C 6 H 12 O 6 +HCN. Amygdalin Benzaldehyde Dextrose Hydrocyanic acid Emulsin is found in many molds and bacteria, and recently has been found in yeasts. Glucoside-splitting enzymes play an important role in the fermentations of coffee-beans, cocoa, mustard and indigo. In most of these fermentations, however, the emulsin is probably not formed by microorganisms, but by the plant, from which the ferment- ing material is derived. ENZYMES OF FATS. All the enzymes acting on fat, decompose it in the same manner; the fat molecule takes up three molecules of water, breaking up into glycerin and three molecules of fatty acid, as indicated on page 112. It is possible that there are several fat-splitting enzymes, but the result of the cleavage process is always the same. The name formerly assigned to enzymes of fat is steapsin, but this term is now almost exclu- 138 NUTRITION AND METABOLISM. sively substituted by the more significant word lipase. Occasionally they are called lipolytic enzymes which expression is analogous to the proteo- lytic enzymes; in the same way, the term amylolytic enzyme is used for diastase. ENZYMES OF PROTEINS. The enzymes decomposing protein bodies, generally called proteolytic enzymes or proteases, have been known for nearly a century. Though the difficulty of analyzing protein bodies accurately prevents an absolute knowledge of proteolysis, much effort has been made to become acquainted with the very important group of en- zymes which accomplish the digestion of protein food. Naturally, most experimenting has been conducted with pepsin and trypsin of the animal body, accordingly these are better understood than others, and only little work has been done with microbial enzymes ; but there is so far as can be determined little appreciable difference between the proteolytic enzymes obtained from different organisms, whether low or high in the plant or animal world, consequently many experiences with animal pepsin and trypsin can be applied to microbial enzymes. The specific chemical action of these enzymes is referable to hydro- lysis; the large protein molecule is broken up into smaller molecules by addition of water. Various proteolytic enzymes differ in the extent of decomposition. While some, like pepsin, produce mainly peptones, trypsin is able to split protein to amino-acids and even to ammonia. Mavrojannis tested for the intensity of gelatin decomposition with formaldehyde. The peptones of gelatin will solidify with formaldehyde while amino-acids are not affected. Proteolytic enzymes were first divided into two groups: pepsins, which act best in slightly acid solutions, and trypsins, which act best in slightly alkaline media. The names are derived from pepsin (peptase), the pro- teolytic enzyme of the animal stomach, and from trypsin (tryptase) which is found in the small intestine of animals. This classification cannot be used for the enzymes of microorganisms because there is no definite line established by the acidity. Some enzymes work in either acid or alkaline media equally well, preferring a neutral reaction. Enzymes should be classified according to the substances they act upon or perhaps according to the nature of the products resulting from the fermentation. This would bring pepsin and trypsin into one class, both acting upon protein bodies as such; they, however, differ in the intensity of action as shown by their products, the pepsin forming mainly peptones, the trypsin carrying MECHANISM OF METABOLISM. 139 on the decomposition as far as amino-acids and traces of ammonia. Another class recently recognized is ereptase (erepsin) which cannot decompose protein, but readily attacks peptones, decomposing them much in the same way as trypsin. Pepsin, trypsin and erepsin do not break up amino-compounds. The presence of proteolytic enzymes in microorganisms is readily tested by cultivation on nutrient gelatin. The proteolytic enzyme secreted by the cells will liquefy the gelatin. Generally, an organism that liquefies gelatin will also decompose the casein of milk and the protein of blood serum. There are some exceptions, however, as is shown in the following table, after Frost and McCampbell. A + sign means proteo- lysis, a sign means no action. Organism. Milk. Coag. Digest. Gelatin. Serum. Fibrin, album. Bact. anthracis Microspira comma M. pyogenes var. aureus. Pseudomonas pyocyanea. . B. violaceus B. mycoides B. prodigiosus A spergillus niger A spergillus oryztz Apparently not all organisms which liquefy gelatin are able to de- compose egg albumin, and we must conclude that the enzyme liquefying gelatin is different from the proteolytic enzyme dissolving egg-white. COAGULATING ENZYMES. The blood-clotting enzyme (thrombase) does not occur in microorganisms. Rennet, however, is found in many species. Rennet is extracted from the stomach of calves and pigs and used to set the curd in milk for cheese making. The enzyme acts upon the casein in milk, decomposing it into paracasein and some soluble protein. The time of coagulation depends upon the temperature of the milk and the concentration of the rennet. This coagulation of milk is quite different from the acid curd, where the insoluble casein is precipi- tated by the acid. If enough acid is added, the milk curdles immediately ; 14 NUTRITION AND METABOLISM. if there is not enough acid, there will be no curd, not even after a long time. An acid curd can be brought back to the original state by an ad- dition of alkali, while a rennet curd by no means can be changed back to casein. Rennet-forming bacteria are found in milk and dairy products, in soil and other habitats. They will coagulate milk without causing any appreciable increase of acidity. They all seem to digest the curd after it is formed (see the above table). The relation between proteolytic and rennet enzymes will be discussed in a later chapter. Rennet is sometimes called chymosin; the Society of American Bac- teriologists uses the German word "lab." ZYMASES. The zymases are the agents which furnish the energy for cell life by causing fermentative decompositions. As has been stated before, the processes which provide for energy must take place inside of the cell. Consequently, all intracellular enzymes are endo-enzymes. The difference between the soluble enzymes and the endo-enzymes is very plainly shown in the following table, giving the energy liberated by the various enzymes by acting upon i g. of substance. Energy liberated from I g. of substance. Soluble Enzymes. Endo-Enzymes. Pepsin, trypsin o calories Lactacidase 82 calories Lipase 4 calories Alcoholase 160 calories Maltase, invertase. . . . 10 calories Urease 239 calories Lactase. . . 23 calories Vinegar-oxidase 2,520 calories The microbial cell does not lose much energy by the activity of the soluble enzymes outside of the cell, because their energy yield is insignifi- cant. The first zymase recognized as such was urease, the enzyme which changes urea to ammonium carbonate. The urease was not considered an exceptional case, and no particular attention was paid to the fact that it was the only zymase known at that time. The actual investiga- gations of the zymases did not start until Buchner had demonstrated that yeast can be ground with infusorial earth until all cells are lacer- ated, and then can be pressed and the juice filtered without losing the power of alcoholic fermentation. Such fermentation cannot be due to MECHANISM OF METABOLISM. 141 anything but a soluble compound of the yeast cell. Thus the alcoholase was recognized. It was found later that yeast may be killed by alcohol, ether or acetone without losing its fermenting power. This last method was applied later to lactic bacteria, and it was proved that the lactic acid is also produced by an enzyme, lactacidase. It is possible to kill the lactic bacteria cells so that they do not multiply but still continue to form acid. It seems quite probable that other fer- mentations of carbohydrates, like the butyric and the gassy fermentations, are really due to enzymes. It is very difficult to give the experimental proof, however. These enzymes are so sensitive that it requires much experience to separate them from the cell, and it is also quite difficult to obtain bacteria in quantities large enough for such experiments. The vinegar oxidase is an enzyme which remains in the cell of the acetic bacterium, oxidizing alcohol to acetic acid. Its independence of the living cell has been demonstrated by killing the cells with acetone. The PROTEOLYTIC ENDO-ENZYMES of yeasts, only, have been studied extensively. That such enzymes exist is recognized by the observation that certain microorganisms do not liquefy the gelatin until after they are dead and the proteolytic enzymes diffuse out through the deteriorating cell membranes. That yeast in the absence of sugar loses in weight, and that leucin and other cleavage-products of protein are formed, was the first indication of a proteolytic process in the yeast cells. By pressing the juice out of the ground yeast cells, a liquid is obtained which liquefies gelatin, digests casein, albumin and fibrin. The living yeast cell does not attack these compounds, because they cannot diffuse into the cell and the enzyme cannot diffuse out. The proteolytic endo-enzyme of yeast is called endo-tryptase. Its object is apparently the regulation of the pro- tein-content of the cell and perhaps it has some bearing on the formation of cell plasma. The possible relation between enzymes and growth is discussed in a following sub-chapter. " If yeast is mixed with a weak antiseptic (chloroform, toluol) the pro- teolytic process takes place quite rapidly. This process is called autolysis (self-digestion). Similar autolytic enzymes are found in other micro- organisms. Autolysis is a well-known process in the higher animals. To this is due the ripening of meat. Proteolytic endo-enzymes must be expected in all microorganisms which depend upon protein as food material only. These organisms will produce certain enzymes which diffuse out of the cell and decompose 142 NUTRITION AND METABOLISM. the protein into bodies which diffuse easily into the cell. Here, proteoly- tic endo-enzymes further decompose these products. Such an endo- enzyme is the amidase discovered by Shibata in the mycelium of Aspergil- lus niger which forms ammonia from urea, acetamid, oxamid, biuret. Endo-erepsin and amidase were also found in Penicillium camemberti by Box. Similar to these proteolytic enzymes is the urease which is formed in large quantities in the so-called urea bacteria, but it is also present in the mycelium of some molds. An endo-enzyme, splitting hippuric acid into benzoic acid and glycocoll, is found in the mycelium of a few molds. OXIDIZING ENZYMES. The most typical example of an oxidizing enzyme is the vinegar- oxidase, because its chemical action is well known. Most of the oxidases known act upon complex organic compounds, changing them to colored bodies. Such an oxidase is the tyrosinase, which forms a black, insoluble compound in tyrosin solutions. It is produced by several bacteria, especially by chromogens, and its application in testing for small quantities of tyrosin has been suggested. A number of oxidases are known to act upon the leuco-bodies of certain organic dye-compounds, as aloin, guaiac, phenolphthalein, and others. Hydrochinon is oxidized by the dead cells of a few molds. Strange seems the oxidation of potassium iodide to iodine by the endo-oxidase of a mold. Many other oxidations are supposed to be of enzymic nature, but their independence of the living cell has not been proved. Many higher organisms are known to contain oxidases, the best studied are those of certain mushrooms which change the white mush- room meat into a bluish or brownish color as soon as it is exposed to the air. Oxidases are very common in most of the tissues- of higher animals. REDUCING ENZYMES. Among the reductases, one enzyme stands apart from all the others, that is the katalase or peroxidase which reduces the hydrogen peroxide to water by liberation of oxygen. H 2 O 2 + katalase =H 2 O+O Katalase is one of the most commonly found enzymes; it is formed by practically all plants and all animals and is contained by all but a few ' MECHANISM OF METABOLISM. 143 bacteria. Among these exceptions is the Bad. lactis acidi. The ab- sence of katalase in this species has been recommended as a diagnos- tic test. It is possible that this enzyme is necessary for intracellular oxidations. A number of other reductases are known. Nearly all of the reductions mentioned in the paragraph on the products of mineral decomposition are proved to be of enzymic nature; these processes will take place after the cell is killed by a disinfectant or is ground to pieces. This can be readily demonstrated by lacerating the cells with quartz sand. They will then reduce nitrates to nitrites, sulphur to hydrogen sulphide. The decolorization of litmus, methylene blue, indigo, and other organic dyes is due in microbial cultures to enzymes which are almost exclusively endo-enzymes. ADDITIONAL REMARKS ON THE RELATION OF CELLS AND ENZYMES. Enzymes are produced only by living cells. After they are once formed, they act like chemical compounds, independent of the cell which produced them. Even the endo-enzymes follow only the law of enzyme action and are not influenced by the cell which contains them. The enzymes are mostly influenced by their own products, and when a certain yeast ceases to ferment sugar at the concentration of 8.5 per cent of alchohol, this means that the alcoholase of this yeast cannot tolerate more than 8.5 per cent of alcohol. The inability of the cell to regulate enzymic action may account for the fact that often a culture produces an amount of fermentation products sufficient to kill all cells. This is ob- served in the lactic, acetic and alcoholic fermentations, and perhaps occurs in many others. Most cells produce more than one enzyme. Microorganisms feeding upon various foods must form various enzymes. Frequently several enzymes are necessary for the decomposition of one compound. Mucor rouxii uses three enzymes in order to form alcohol from starch, first the diastase to change starch to maltose, then maltase to change maltose to dextrose and finally alcoholase to change dextrose to alcohol and carbon dioxide. The number of enzymes formed by certain microorganisms is surprising. Aspergillus niger has the reputation of forming almost all enzymes which have ever been found in microorganisms. Penicillium camemberti produces (after Dox) erepsin nuclease, amidase, lipase, 144 NUTRITION AND METABOLISM. ' emulsin, amylase, inulase, raffinase, invertase, maltase and lactase. It has been believed for a long time that certain enzymes are regular products of the cell while others are formed only if the substance upon which they act is present. According to Dox's investigations with Penicillium camemberti, there is no evidence that enzymes not normally formed by the organism in demonstrable quantities can be developed by special methods of nutrition. The addition of a particular food compound does not develop an entirely new enzyme, but stimulates the production of the corresponding enzyme which is normally formed, although in small amounts, under all conditions. THEORY or KATABOLISM. Regarding katabolism as the sum of all destructive processes of the living cell substance, i.e., of the protoplasm, and considering the cell substance to be decomposed and renewed constantly as long as the cell is performing the normal functions of life, then there must be a reno- vating and a destructive process continuously going on in the proto- plasmic molecules. If the food supply ceases, anabolism ceases with it, but it has been demonstrated that katabolism may continue just the same for some time. By this method, the products of katabolism can be obtained free from the products of food digestion which would obscure the results of experiment with katabolism in normally fed cells. It is difficult to determine to what extent katabolism is controlled by endo-enzymes, the so-called autolytic enzymes, which have been mentioned in the above paragraph. In the autolysis of yeast cells, the only well- studied example of microbial autolysis, have been found guanin, adenin, xanthin, hypoxanthin and ammonia. THEORY OF ANABOLISM. INTERACTION OF ANABOLISM AND INTRA-CELLULAR FERMENTATION. All changes discussed in the previous chapters are fermenting pro- cesses in which organic or inorganic compounds are broken up to smaller molecules. These processes are exothermic, i.e., liberating heat or energy in other form. The opposite is true of the anabolic processes which build up complex molecules from simple compounds. These synthetic processes are endothermic, absorbing heat or energy in other MECHANISM OF METABOLISM. 145 form. Growth is the typical manifestation of anabolism. It is the formation of new cells from dead organic or inorganic matter, and it means the formation of all the compounds necessary for cell life. Of all the substances found in the cell, practically none are contained in the food, and it is wonderful that in such a small unit as a microbial cell, there are contained the powers of making protoplasm, enzymes, nuclear bodies, chromatin-bodies, the substance of the cell wall and probably many other unknown compounds. All these complex substances are generally made from simple food compounds as amino-acids, carbo- hydrates and others. These synthetic processes of the cell will, like most endothermic processes, take place only if energy is provided. This condition is usually fulfilled in the living cell, due to the fermenting processes going on con- tinuously. There is a strange interaction between anabolism and intra- cellular fermentation proceeding in the protoplasm and this linking together of destructive and constructive reaction is the basis of life processes. The life processes decompose certain substances, the energy liberated allows the formation of protoplasm, which again liberates energy. Thus a continuous formation of protoplasm is secured. An explanation of anabolism based upon chemical experiments is not possible at the present time. In the study of intra- cellular destruction it is possible to trace most processes back to enzymic action. There our knowledge ceases because the nature and mode of action of enzymes is unknown. In the study of anabolism our knowledge has not even progressed so far. The most promising explanation at present is based upon the reversibility of enzymic action. REVERSIBILITY OF ENZYMIC ACTION. Chemical reactions between organic compounds proceed quite rapidly at first, then become slower and slower until the reaction stops entirely. The reaction is not com- plete at the time it reaches an equilibrium. If the equilibrium is disturbed by adding more of the reagents, the process will continue. If, however, the products of reaction are added, the reverse process will take place. Reactions between organic compounds can proceed either way, depending upon the relative concentrations of the reacting substances. The stand- ard exaniple is esterification. Acetic acid plus alcohol gives ester plus water, CH 3 COOH+ CH 3 CH 2 OH<=>CH 3 COO CH 2 CH 3 + H 2 O Acetic acid Alcohol Ester 10 146 NUTRITION AND METABOLISM. The process goes to a certain equilibrium and stops. If ester is mixed with water, it gives acid plus alcohol, until the same equilibrium is reached. If acid and alcohol are added to. a system in equilibrium, more ester will be formed. If ester is added, more alcohol and acetic acid will be formed. The same is true with enzymes, at least with some enzymes. Maltase will decompose maltose into two molecules of dextrose. In a concentrated solution of dextrose, however, maltase will form maltose, or a similar sugar, isomaltose. Lipase is able to produce fat from glycerin and fatty acids. A solution of albumose with trypsin or pepsin gives a precipitate of a body which is more complex than albumose and which gives the protein reactions. It is believed by many physiologists that pepsin and rennet are the same body. Under certain conditions, it has a dissolving power, under other conditions it has the power to coagulate. The reversibility of enzymic action has given rise to much speculation about assimilation and growth. It seems reasonable to suppose that the cell forms its protoplasm from amino-acids by the reversed action of proteolytic enzymes. In the same way, cellulose may be formed from dextrose, fat from glycerin and fatty acids. Nearly all phases of growth can be accounted for in this way. This is nothing but theoretical specu- lation, and the only fact to support it is the reversibility of certain enzymes. The conditions under which chemical reactions take place inside of the cell are very largely unknown. There are so many processes going on at the same time that it is absolutely impossible at the present time to obtain a perfect knowledge of all these reactions. Our experience is limited to the very simplest changes, and even these are not perfectly understood because the detailed conditions under which the changes take place are unknown. Information obtained by experiments in vitro is practically all that is available, and these experiments are conducted under very simple conditions, where complications as they might occur in the cell, are excluded. Thus, our knowledge of the processes of growth is largely based upon analogy and speculation. DIVISION II. PHYSICAL INFLUENCES. CHAPTER I. MOISTURE. Moisture may be called the most important factor of life. Not only bacteria, but every microscopic and macroscopic being requires a con- siderable amount of moisture. Living organisms contain on the average between 70 per cent and 90 per cent of water, and only 10 per cent to 30 per cent of solid matter. Microorganisms which live entirely submerged in liquids need water not only within but without the cells. Bacteria, yeasts, molds, and some protozoa obtain their food by diffusion through the cell-membrane; their food-substances must be soluble and dissolved. No other liquid can take the place of water. The amount of water required by microorganisms cannot be stated briefly. Several factors have to be taken into consideration, as the osmotic pressure, the insoluble and the colloidal substances, the species of organisms, temperature, and perhaps others. OSMOTIC PRESSURE. In the organic world we find very commonly membranes which will allow water to pass through but retain some compounds dissolved in the water. Such so-called semi-permeable membranes are found surrounding the protoplasm of cells. They are not the cell wall, but separate the protoplasm from the cell wall. Similar properties are found in parchment paper, pig's bladder, and other organic membranes. If a salt solution is poured in water, the two liquids will mix in a short time and soon every smallest portion of the mixture will have the same concentration. If a salt solution and water are separated by a membrane which does not allow the salt to pass, the water will go through the membrane toward the salt with a certain amount of pressure. This pressure depends upon the nature of the dissolved substance as well as upon its concentration. 147 148 PHYSICAL INFLUENCES. The pressure increases in direct ratio with the number of molecules in solution. Therefore, the pressure of solutions of equal concentration by weight will be the smaller the larger the molecule, because the larger the molecules the smaller the number required to make a certain weight. The osmotic pressure of protein, starch and peptone solution can be measured only with the finest instruments, while the pressure of a 30 per cent dextrose solution is 22 atmospheres.* With acids, alkalies and salts, the pressure is higher than would follow from the concentration, because the molecules of these electrolytes are dissociated, thus increasing the number of unit-particles in solution. PLASMOLYSIS. If a cell is brought into a strong solution of a substance which cannot pass the plasma-membrane, this substance will cause an osmotic pressure and the concentration in the cell being lower than in the medium, the water will pass out from the cell until the pressure inside and outside is the same. This causes a shrinking of the protoplasm, while the rigid cell wall keeps its shape. Such plasmolyzed organisms are illustrated in figure 30, p. 50. While plasmolysis is easily demonstrated with the cells of higher plants, microorganisms do not show it so readily. In fact, many bacteria, like B. subtilis, Bact. anthracis, cannot be plasmolyzed by any concentra- tion of salt in solution. Others, as B. coli, B.fluorescens react promptly. But even though many are killed, the rest recover from plasmolysis after a few hours, and appear normal. This indicates that the salt passes slowly through the plasma membrane and thus increases the pressure inside the cell until finally the inside and outside pressure are the same again. The fact that many microorganisms show no plasmolysis whatever is explained in the same way. These organisms probably have plasma- membranes so constructed that the salts diffuse through nearly as fast as the water. An absolute exclusion of all soluble substances by the mem- brane is impossible since the food can get into the cell only by diffusion through the membrane. The resistance of various microorganisms against concentrated solutions depends upon the organism as well as upon the dissolved sub- stance. The sodium and potassium salts of the common mineral acids act upon a culture nearly in proportion to their osmotic pressure, but the potassium salts always retard growth a little less than the sodium salts. * One atmosphere equals the pressure of one kilogram per square centimeter or about 1 5 pounds per square inch. MOISTURE. 149 The effect of salts upon microorganisms is therefore not due to the os- motic pressure only; the chemical constitution of the salts also plays an important role. The different functions of life are influenced in different degrees by concentrated solutions. Some bacteria will multiply but not form spores in salt solutions. Molds will sometimes show a good growth in concen- trated sugar solutions but fail to produce spores unless the medium is diluted. Bact. anthracis loses its virulence in sea water. Often the form of microorganisms is affected by concentrated solutions. Some bacteria grow more spherical, others become elongated or distorted. The deforming influence is not due to the osmotic pressure only, but depends mainly upon the chemical character of the salt; magnesium salts especially have a tendency to produce such involution-forms. Salt and Sugar Solutions. Most experiments on the influence of concentrated solutions have been carried on with sodium chloride, be- cause of its wide application in the preservation of foods. Most micro- organisms, especially the rod-shaped bacteria, are suppressed by a salt concentration of 8-10 per cent. At 15 per cent only few cocci develop slowly, while some species of torulae grow without a very noticeable re- tardation. Above 20 per cent the torulae are practically the only organisms which can develop. They are, therefore, found in all food products which are preserved by salt, as salted pork, beef, fish, butter, and pickles, often in nearly a pure culture. It seems that they are easily overpowered by other organisms in the absence of salt, but this has a selective action, preventing nearly all other organisms but the torulae. The selective influence of salt is used in some fermented products to prevent undesirable fermentations. This is true in sauerkraut and brine pickles, where the desirable bacteria can grow in the presence of salt while the undesirable ones are kept away. Possibly the salting of butter has the same effects. Another compound of great practical importance is cane sugar, which is the standard preservative for fruits and condensed milk. Its action has been studied mainly upon molds. Theoretically, dextrose should be expected to have twice as strong a preserving action as saccha- rose because it has only half the molecular weight and consequently produces twice as strong an osmotic pressure in the same percentage of concentration. But though its preserving action is a little higher than that of saccharose, the proportion is not nearly 1:2. The common molds 150 PHYSICAL INFLUENCES. are extremely resistant to strong sugar solutions, about 60-70 per cent of cane sugar seems to be the limit of growth for Penicillium and Asper- gillus species. Yeasts can also grow and ferment in very concentrated solutions while bacteria in general do not tolerate solutions higher than 15 to 30 per cent, though many exceptions are known. Colloidal Solutions. In order to determine the amount of water which is absolutely necessary for microbial proliferation, only such media can be used which do not cause osmotic pressure. If B. prodigiosus does not develop in a 10 per cent salt solution, this is not due to lack of moisture, because the same bacillus will grow in a 30 per cent sugar solution which contains 20 per cent less moisture. Another factor be- sides the water content enters, which can be avoided only in solutions without osmotic pressure. A few substances are known to give such solutions. It was stated before that the osmotic pressure depends upon the number of molecules dissolved in a liquid; the larger the molecule the lower the osmotic pres- sure. There is a group of substances known as colloidal bodies which have a very large molecular weight, between 1,000 and 1 0,000, it is estimated. Their osmotic pressure even in very concentrated solutions would not be high enough to interfere with microbial growth. Among these colloidal bodies are found egg albumin, gelatin, peptones, all protein substances; also starch, dextrin and gum arabic among the carbohydrates. None of these substances has a retarding influence upon bacteria; some of them can be mixed with water in all proportions; consequently, they are the ideal medium to test the water requirements of microorganisms. Experiments carried on with gelatin, powdered meat, crackers, bread and potato, vary but little in results. A few bacteria cannot grow in a medium with only 60 per cent water, but most organisms develop slowly even with 50 per cent water and some may be able to develop with only 40 per cent. Molds can grow very scantily in even more concentrated media. Protozoa probably have to have a more diluted medium for their development though no experiments bearing upon their water requirements are known to the author. The fact that in a colloidal solution growth will cease if the moisture is below 30 to 40 per cent does not necessarily indicate the conclusion that any substance with less than 30 per cent water cannot be decomposed. The above statement refers only to solutions, while in natural media as dried foods or soil, a combination of solid and dissolved substances is in- MOISTURE. 151 volved. Butter is an excellent medium for many bacteria, yeasts, and molds, though it contains only 12 to 15 per cent of moisture. If butter fat were soluble in water, the concentration of 85 parts of solids in 15 parts of liquid would certainly prevent any growth whatever, but fat is insoluble, and the fat particles do not interfere at all with the growth of microorgan- isms in the droplets of buttermilk distributed all through the butter. The concentration in these small droplets is the deciding factor. If the growth of microorganisms in butter is to be prevented by salt, it is un- necessary to give any attention to the fat; the bacteria live only in the water and not in the fat globules. In adding 3 per cent of salt to a butter with 15 per cent of moisture, a brine of 3 parts of salt in 15 parts of water is produced; in other words, a 20 per cent brine, because salt does not dissolve in the fat. Similar considerations will come up in the preserva- tion of fruit, vegetables, meat, milk, and other food substances by drying or condensation. DESICCATION. Microorganisms do not die immediately if water is not present. The majority of bacteria will remain alive for a few days if dried on glass or filter-paper. Some will live for a month or more, while a few, like the B. carotamm, die within twenty-four hours after drying. Spores of bacteria are extremely resistant to desiccation. Certain spores, like those of Bad. anthracis and B. mesentericus, have been kept alive for many years. The mycelium of molds is ordinarily killed if dried com- pletely, while the spores survive. Yeasts show a varying resistance. The resistance of microorganisms is influenced greatly by the medium on which they are placed for drying. Hansen found that yeast cells dried on cotton were still alive after two to three years, while if dried on platinum wire some died in five days and others lived as long as 100 days. Compressed beer yeast mixed and dried with powdered charcoal kept as long as ten years; Pseudomonas radicicola dried on a cover-glass or filter- paper died within twenty-four hours; on seeds, this same organism was still alive after fourteen days and in the dried nodules of legumes a few cells were able to reproduce after more than two years. Soil containing an average number of 17,000,000 bacteria per g. was dried for two years; the total number of organisms averaged then 3,250,000; 20 per cent of the bacteria, therefore, could resist desiccation. Dried cultures of microorgan- isms are commonly sold for several purposes, as dairy-starters and the so- called "magic yeast" used for bread-making. Such cultures are dried on milk, sugar, starch, flour or similar porous and absorbing material. Starters 152 PHYSICAL INFLUENCES. are usually guaranteed only for a certain length of time, from one to twelve months. The advantage of the dry culture is its better keeping qualities. Liquid cultures produce substances harmful to themselves, and die rapidly after a short time, while the dry cultures show little change. The resistance of pathogenic bacteria to desiccation is of considerable importance in the spreading of contagious diseases. Many pathogenic bacteria die after desiccation of a few hours to a few days, and spreading of such diseases by dust is highly improbable. Protozoa of soil decrease in number 'by drying, but all are not killed. CHAPTER II. INFLUENCE OF TEMPERATURE. Temperature, as well as moisture, is one of the most important factors of life. It is so important that the most highly developed animals pro- tect themselves by a very complicated mechanism of regulation against changes of temperature; the life processes of such animals will take place at a temperature nearly constant from birth to death. This neces- sitates a distinct difference in the metabolism of warm-blooded animals and all other organisms. The metabolism of the warm-blooded animals takes place at a constant temperature. The required amount of food is constant except for the part that is used for heating the body; at lower temperatures, more heat-producing material is used and the result is that warm-blooded animals require more food, the lower the temperature. All other organisms, reptiles as well as bacteria, have the temperature of their environment and the decrease of temperature will decrease the intensity of metabolism as it retards any other chemical process. The lower the temperature, the less food is required by all lower organisms. There are, of course, limits to the favorable influence of high tempera- ture. Growth and metabolism of microorganisms will increase with a rising temperature to a certain point, called the optimum temperature, and beyond this point the rate of growth will fall off rapidly and soon cease entirely. The highest temperature at which growth can take place is called the maximum temperature. Correspondingly, the minimum temperature of an organism is the lowest point at which growth can take place. THE OPTIMUM TEMPERATURE which allows the fastest growth will be quite different for different species. Groups of bacteria are known which develop only at very high temperatures and others for which room tem- perature is too high. The temperature requirement is largely dependent upon the natural habitat of the organisms. The bacteria of the polar sea and of a lagoon near the equator will very probably have different optimum temperatures because of the acclimatization and selection which has been taking place for centuries. 153 154 PHYSICAL INFLUENCES. The great majority of bacteria and related organisms, in fact of all living organisms, has its optimum temperature between 20 and 40. The optimum temperature of an organism is generally somewhat higher than the average temperature of its natural habitat. This will be in most instances between 10 and 38. A few examples will illustrate this. The bacteria of animal diseases are accustomed to body temperature and grow best at 37 to 40. The organisms found in soil are of various natures. Since good soil in summer under the direct radiation of the sun quite often reaches high temperatures, a great number of soil bacteria will have their optimum nearer 40 than 30. The ordinary lactic bacteria of milk and many of the water bacteria have their optimum near 30. Most of the common molds grow best between 20 and 30. Only very few can grow at body temperature. The optimum temperature of some water bacteria is quite low, the best-known example being perhaps the photogenic bacteria (page 129). The following table shows the data obtained for a few microorganisms. Temperatures Species Minimum Optimum Maximum Penicillium glaucum i S 2C-27 , i-?6 A spergillus niger 7-io f s * I ,,0-0 o- 1 o u 4O-41 Saccharomyces cerevisicz I i-* oo o/ 28- 70 40 Saccharomyces pasteurianus I S 2 e-o O ^4 Bacterium phosphoreum "' J below o "j O u i6-i8 OT- 28 Bacillus subtilis 6 30 r Bacterium anthracis 10 o" , o_, 7 o O u 4 , Bacterium ludwigii to O" O/ rr-r7 ^o 80 THE MINIMUM TEMPERATURE or the lowest limit of growth is usually farther from the optimum than the maximum temperature. It will vary with the organisms just as do the other cardinal points. But there is a natural limit drawn by the freezing-point of the nutrient liquid. Not all organisms can grow at such low temperatures, in fact the greater number does not develop below 6 to 10. Those that can grow near the freezing- point will be inhibited by the solidification of the water in the nutrient medium, for if the water is frozen, food cannot diffuse into the cells and INFLUENCE OF TEMPERATURE. 155 therefore all life processes are checked. If freezing is prevented by adding salts or other soluble substances which lower the freezing-point, growth may continue even below o. Milk freezes at about 0.5. Bac- teria are found to multiply in it as long as it is not entirely solid. A certain yeast multiplied slowly in salted butter kept at about 6. The number of microorganisms that developed at the freezing-point was found to be in i c.c. of market milk, up to 1,000 germs. in i c.c. of sewage, up to 2,000 germs, in i g. of garden soil, up to 14,000 germs. THE MAXIMUM TEMPERATURE is usually about 10 to 15 higher than the optimum. The development of microorganisms above the optimum temperature is not quite normal; there is a great tendency toward invo- lution forms. The mycelium of molds grown near the maximum tem- perature appears unhealthy and pathogenic bacteria lose part of their virulence. This loss of virulence is made use of in the preparation of attenuated cultures for vaccines. The maximum temperature varies with different species of bacteria. Most bacteria do not grow above 45, but with some the maximum temperature is considerably lower. Bact. phosphoreum dies if exposed for a few hours at 30; others may require still lower temperatures. The average organisms found in water, soil, milk, and the body, which have their optimum near 30 to 38, do not grow higher than about 45. There are very noticeable exceptions to these, such as the physiological group known as thermophile bacteria. These extraordinary organisms have their maximum between 70 and 80, a temperature which coagulates albumin. Corresponding to the high maximum the thermophiles have a very high optimum, and the minimum lies with most of these species above 30. These organisms are found in soil, sewage, ensilage and occasionally in milk. They find the temperature suitable for their life only under extraordinary circum- stances, as in fermenting manure piles, in silos, in self-heating hay and similar organic material that develops a high temperature by fermenta- tion. Some hot springs have a very remarkable flora of thermophile bacteria. BIOLOGICAL SIGNIFICANCE OF THE CARDINAL POINTS OF TEMPERA- TURE. The importance of the temperature requirements of certain organ- 156 PHYSICAL INFLUENCES. isms to the r61e they play in nature can be illustrated by a few examples. Most molds cannot cause disease in man and warm-blooded animals because their maximum temperature is below the body temperature. Exceptions are some A spergilli and Mucors. Pathogenic microorganisms must have their optimum temperature coincide with that of their host. Organic substances may undergo a different change at different temperatures. The biochemical changes in soil may not be the same in northern Canada and near the Gulf of Mexico. Even the warm and cold season of the same climate is apt to change not only the rate of decomposition but possibly the products. Perhaps the most striking example in this respect is the decomposition of ordinary market milk kept at different temperatures. Such milk contains a great variety of microorganisms; at various temperatures different types will predominate, while the remainder are retarded or inhibited by unfavorable temperature conditions and by the products of the dominant type of bacteria. If milk is kept at about the freezing-point, only a few organisms will develop slowly, but after a certain time their number will increase to many million cells per c.c. There is, however, no apparent change ; no acid or deteriora- tion can be discovered by the taste though chemical analysis proves the presence of hydrogen sulphide and ammonia. Between 15 and 25, milk will sour in about thirty-six to forty-eight hours, giving a firm curd of an agreeable flavor without whey or gas; later Oldium lactis destroying the acid develops on the surface. Near body temperature the milk will lopper in twenty-four hours, the curd is usually contracted, a large quan- tity of whey is extruded, and much gas is produced by Bad. aerogenes and B. coll. The odor is disagreeable and later butyric acid is produced; eventually the lactic acid increases further by the action of Bad. bulgaricum If kept above 50 the milk usually keeps for twenty-four hours, but after that a decomposition by thermophile bacteria begins which is either an acid fermentation followed by digestion or a complete putrefaction depending upon the species of thermophile organism that happens to be in the milk sample. Thus there is in the same substance, containing the same organisms at the start, four entirely different types of decomposition induced only by the difference of temperature. This indicates the importance of temperature regulation in the fer- mentation industries. Even pure cultures may give different products if working at different temperatures. Cream ripened with a pure culture starter at too high a temperature will have a sharp acid flavor. The cold INFLUENCE OF TEMPERATURE. 157 curing of cheese has become a very common practice because of the much improved flavor. Bioletti claims that the value of the dry California wines would be doubled if the fermentation were carried on generally at a lower temperature. In the chapter on enzymes it was stated that the fermentations were due to enzymes which are independent of the cell after they are once produced. The question arises whether the optimum temperature of growth coincides with the optimum temperature of fermentation. Too little is known as yet about the nature of enzymes to make definite statements. END-POINT OF FERMENTATION. Another question is the relation between the end-point of fermentation and the temperature. Of the few data existing, many indicate that at a lower temperature the final fermentation goes farther than at a higher temperature. Miiller- Thurgau found that under exactly the same conditions with the tempera- ture as the only varying factor the following final amounts of alcohol were produced by a pure culture of yeast. at 36 3.8 per cent alcohol. at 27 7.5 per cent alcohol. at 18 8. 8 per cent alcohol. at 9 9.5 per cent alcohol. Concerning the lactic fermentation some investigators find no difference in the end-point, while others obtained results similar to the results with alcohol. With three strains of Bad. lactis acidi were obtained after thirty- four days, A. B. C. at 37 0.89 per cent 0.87 per cent 0.60 per cent of lactic acid, at 30 i. oo per cent 0.96 per cent o. 8 1 per cent of lactic acid, at 18 i. 08 per cent 1.06 per cent 0.88 per cent of lactic acid, at 6 0.70 per cent 0.73 per cent 0.62 per cent of lactic acid. These results are quite logical and perhaps can be explained by the recognized experience that all products of fermentation tend to check the process of fermentation, and that any chemical product or substance acts the more vigorously upon any life process the higher the temperature. The same amount of alcohol that will still allow a slow fermentation at 10 may check the fermentation entirely at 20. Naturally the rate of 158 PHYSICAL INFLUENCES. fermentation in the beginning will be higher at the higher temperature but the end-point is lower. The end-point of the lactic cultures A, B, and C at 6 is probably not final, because thirty-four days is a short time of growth at so low a temperature. Above the optimum the rate of decomposition will decrease rapidly with the rising temperature and the end-point will also be lower. As already mentioned above, pathogenic bacteria lose to some extent their virulence, that is, the power of producing disease, if grown above their optimum. FREEZING. The discussion of the relation of temperature to micro- organisms has so far considered only the temperatures within the limits of growth. However, the temperatures below the minimum and above the maximum are also of greatest importance. If bacteria are cooled be- low their minimum temperature they do not die immediately (except a few thermophile bacteria) . They remain alive in a dormant condition ready to multiply as soon as the temperature rises. Even the freezing of a liquid will not kill them immediately. Of course, they cannot multiply in ice, because they have no water, consequently no food, and they cannot thaw the ice to get their water and food for lack of body temperature of their own. As long as liquids are frozen solid the bacteria in them will remain dormant much like dried organisms, and like them their number will decrease very slowly. If ice has been kept frozen many months, it may be sterile, while the fresh ice has nearly as many bacteria as the water it came from. An example is given in the following table relevant to the number of bacteria in frozen milk (after Bischoff). Milk kept at 3 to 7. Freshly frozen 200,000 bacteria per c.c. After i day 105,500 bacteria per c.c. After 2 days 7 2 ,3o bacteria per c.c. After 3 days 62,000 bacteria per c.c. After 4 days 46,400 bacteria per c.c. After 7 days 44,000 bacteria per c.c. After 14 days 40,50 bacteria per c.c. After 21 days 30,300 bacteria per c.c. After 35 days 22,500 bacteria per c.c. After 49 days 14,200 bacteria per c.c. The table shows plainly that it is impossible to sterilize milk by freez- ing, but as long as it is frozen it will keep; there is no possibility of any microorganisms decomposing a frozen liquid, for the organisms need INFLUENCE OF TEMPERATURE. 159 water above all. If food substances change in cold storage (and some food products do deteriorate), this must be either due to changes other than microbial or the material was not completely frozen as is probably the case with salted butter. After bacteria are once frozen, they do not seem to be affected by any lower temperature. Macfadyen and Rowland found that they tolerate very low temperatures remarkably well. Many bacteria were not killed by a twenty-hours' exposure to the temperature of liquid hydrogen (-252). Yeasts are not quite so resistant and the mycelium of most molds is easily destroyed by freezing, while the spores are hardier. THERMAL DEATH-POINT. Heating above the maximum temperature is decidedly harmful to microorganisms; if the exposure to such unsuit- able conditions is prolonged for a certain length of time, it results in the death of the organism. The length of time required to kill a certain organism will depend mainly upon how high the temperature is above the maximum. A few degrees above this point, it will take several or even many hours to kill the organism; the higher the temperature the shorter the time. An exposure to 10 to 20 above the maximum takes generally but a few minutes. It can be stated generally that the lower the maximum temperature the more easily is an organism destroyed by heat. It is customary to speak of the thermal death-point of an organism as the lowest temperature which will kill it within ten minutes. (Instead of this time adopted by the Society of American Bacteriologists, some investigators prefer one or five minutes as the standard time.) The thermal death-point does not depend upon the species and the temperature only. It varies with the age of the culture since older cells are less resistant than younger ones especially if heated in their own pro- ducts. The medium in which the organisms are heated is also of great significance. The fact that acid liquids, as fruit juices, are more easily sterilized than neutral meat or vegetables is largely due to a chemical (poisonous) action of the acids upon bacteria. But the greater resistance of tubercle bacteria in sputum compared with those suspended in salt solution cannot be so readily accounted for. A necessary factor for the prompt destruction of organisms by heat is the presence of moisture. The resistance of dry organisms is remark- ably higher than that of the same organisms in a liquid culture. The following table shows the death-point of yeast cells and spores in a dry and moist state. i6o PHYSICAL INFLUENCES. Thermal Death-point of Dry and Moist Yeast. < ^ells SF ores Variety of yeast Moist Dry Moist Dry Pale ale yeast. 6 <5 CK-IOS 6s-7o Iii5 -i2<5 Hofbrau yeast 55 85- 00 65 II5-I20 Saccharomyces pasteurianus 5o-55 ioo-io5 60 H5 RESISTANCE OF SPORES. The most resistant organisms to heat are the spores of certain bacteria. In the chapter on moisture requirements attention has been called to the great resistance of spores to drying. We find the same exceptional resistance to high temperatures. Boiling heat will not kill spores readily. Some bacterial spores can stand the tem- perature of 100 for several hours. In order to kill spores in one heating the temperature must rise to about 110 for fifteen to thirty minutes; this can be accomplished only by heating under pressure. This is not always advisable for sterilizing food substances. While vegetables are usually sterilized under pressure without losing much of their palata- bility, other foods like milk are changed materially in taste and ap- pearance. To prevent these changes, discontinuous sterilization is sometimes used. This is based upon the following principle: If milk or any other medium is heated to 100 for about fifteen min- utes, all living cells of bacteria, yeasts and molds will be killed except a few spores of bacteria. After cooling, these spores will germinate under suitable conditions and the vegetative cells thus appearing instead of the resistant spores are easily killed in a second heating. A third heating is necessary in order to kill any vegetative cells which may have developed from spores not yet germinated before the second heating. It is essential to have the time between two heatings long enough to allow the germination of spores, and not too long to permit formation of new spores. It is customary to heat on three successive days for fifteen minutes each time. In this case, sterilization is usually complete, while a forty-five minutes' heating at once is not sufficient to guarantee sterilization. Among the substances that are very easily sterilized are cider and other fruit juices, while milk and soil are the most difficult materials to sterilize. Dry spores will resist still higher temperatures than moist spores INFLUENCE OF TEMPERATURE. l6l Some dry spores survive an exposure to 140 to 150 for ten minutes. It requires a very high temperature to sterilize glass, cotton, gauze, and instruments with dry heat. A discontinuous sterilization of dry material is useless since the spores will not germinate without moisture, therefore their resistance remains unaltered. The spores of molds are more resistant than the mycelium but, if moist, they all die at 100. The dry mold spores can tolerate a some- what higher temperature, but not as high as the spores of many bacteria. Yeast spores and yeast cells are very much alike in their resistance to heat. The table on page 160 shows hardly any difference between their resistance. ii CHAPTER III. INFLUENCE OF LIGHT AND OTHER RAYS. Microorganisms in their natural environment are temporarily but not usually exposed to light. The organisms of decay, living in soil, in foods, in the intestines of animals, will only occasionally come in contact with the direct rays of the sun. Water bacteria and the organisms on the surface of plants and animals are more commonly exposed to the sun. The influence of light varies with its intensity. Direct sunlight has a FIG. 52. -These plates were heavily inoculated with B. coli and B. prodigiosus respectively and then were exposed, bottom side up, to the direct rays of the January sun, for four hours. On the instant of exposure, a figure O, cut from black paper was pasted to the plate shading the bacteria underneath. After one, two and three hours, the corresponding figures were pasted to the plates. The above picture was taken 24 hours after exposure, proving that three or four hours of direct sunlight weaken and may even kill bacteria. B. prodigiosus proved more sensitive than B. coli. (Original.) very harmful effect upon microorganisms. Most bacteria are killed by direct sunlight in a few hours; the time depends upon the organism as well as upon the intensity of light; this again varies with the amount of moisture and dust in the atmosphere, with the time of the day and with the season; an absolute measure for the action of light cannot be fixed, 162 INFLUENCE OF LIGHT AND OTHER RAYS. 163 therefore, as easily as with the action of heat in the thermal death-point. The different colors of the spectrum do not act alike; the part of the spec- trum from red to green is practically without influence upon micro- organisms, while the blue light acts strongest and the intensity decreases in the violet and ultra-violet. In carrying on experiments with the in- fluence of light, it must be remembered that glass absorbs ultra-violet rays, and further that the heating of the medium by direct radiation must be avoided. Yeasts, molds, and bacteria and probably protozoa are equally sensi- tive to light. Even the spores of most bacteria do not show a greater resistance to light, while the mold spores are an exception. The colored FIG. 53. Phototropism of Rhizopus nigricans. The mold was grown on gelatin with diffused light coming from right side. (Original.) spores of the Penicillium, Aspergillus and Mucor species can be exposed to light for a long time without being killed, but the colorless spores of Oidium and Chalara show no increased resistance. It is supposed that the pigment in mold spores is a protection against light. This is not true with the pigment of bacteria. The colored and colorless strains of pig- mented bacteria show no difference in their resistance to light. Only one group, the so-called purple bacteria, is an exception. These peculiar organisms, many of which feed on hydrogen sulphide, seem to thrive better in light than without it. Direct sunlight does not kill them, it rather attracts them and they move toward the light. This is called 164 PHYSICAL INFLUENCES. phototaxis or heliotaxis. The pigment, bacteriopurpurin, does not take the place of chlorophyl, however, since the bacteria do not produce oxygen in light and always need organic food. The effect of light upon microorganisms is mainly brought about by a chemical change in the protoplasm, and also, to some extent, by a chemical change in the medium, namely the formation of a peroxide or a similar oxidizing agent. The germicidal action of light is of importance in the purification of rivers. It is applied also in curing diseases of the skin, as lupus and FIG. 54. Two cultures of an Aspergillus, one grown in the dark, the other in diffused light, showing rings. (Original.) leprosy, by exposing the diseased parts to a very concentrated light of the electric arc. This light contains plenty of blue and violet rays and is preferable to sunlight because it is always ready for use and its com- position and intensity can be controlled easily. Diffuse light is not nearly as harmful to microorganisms as direct sunlight. Long exposures to diffuse light will kill most bacteria, while molds are not at all sensitive. They rather like a very dim light, and many molds grown in a dark room with light only from one side will grow toward the light. This property, which is characteristic for all green plants, is called heliotropism or phototropism (Fig. 53). It has been found that molds produce mycelium mostly in the dark, while in daylight sporangia are produced mainly. This difference in the development INFLUENCE OF LIGHT AND OTHER RAYS. 165 during the day and during the night accounts for the concentric rings which are quite commonly found in older mold colonies, and which in- dicate the age of the culture (Fig. 54). Similar rings are occasionally found with yeast and bacterial colonies, and are possibly due to the same influence of light. X-RAYS. Of other rays, the invisible X-rays and the radium rays have attracted the attention of bacteriologists and physiologists. It is known that the X-rays will destroy living tissue by long exposures; microorganisms cannot be considered less resistant. X-rays are used in the treatment of microbial diseases of the scalp and skin. RADIUM RAYS are not so well known, and their bactericidal action is doubtful. The treatment of certain bacterial diseases has been attempted, but it has not been applied as generally as yet as the X-ray method. The sterilization of milk and possibly other foods by this method has been suggested, but the practical application is at present quite improbable be- cause of the cost and the uncertainty of the results. CHAPTER IV. INFLUENCE OF ELECTRICITY. The influence of electricity upon microorganisms is much less than one might perhaps expect, if the electricity as such is considered. A direct electric current passing through a nutrient medium will, of course, cause electrolysis which is usually manifested by the formation of acid on the positive pole and of alkali on the negative pole. The acid and alkali will kill microorganisms, as is discussed in the chapter on chemical influences. In this case, it is not the electricity itself that destroys the bacteria. It is also possible to kill bacterial cultures by passing an alternating current through the medium for some time. No electrolysis takes place in this case, still it is not the direct action of the current that acts upon the organisms, but rather the heat produced by the current passing through a medium of high resistance. If the culture is cooled properly the influence of the cur- rent is insignificant if at all noticeable. Whenever electricity is applied against microorganisms, the effect is considered electrochemical. The electrical current is used in a very small way in the purification of sewage. The sewage passes between two iron plates which represent the two poles of a strong current. The electrical sterilization of milk has been patented. Wines are improved by electricity. The sterilization of drinking water by ozone is also an application of electricity, though of course the ozone once formed by the current acts as a chemical com- pound independent of its source. 166 CHAPTER V INFLUENCE OF THE PHYSICAL STRUCTURE OF THE MEDIUM. The physical structure of the medium has often a remarkable in- fluence upon the development of microorganisms. Very little attention has been paid to this fact, as yet, and only a few instances are known where the structure of the medium is a deciding factor in the life of microorgan- isms. A few examples have already been mentioned. Saccharomyces will only exceptionally form spores on the surface of liquids while they are abundantly formed on the surface of a moist gypsum block. This may be accounted for by the better aeration of the yeast cells on gypsum. Another example, mentioned before, is the influence of the medium, on which bacteria are dried, upon their resistance against desiccation. Chemical action of the medium upon the bacteria cannot explain the differences since the same stratum in different structures gives different results. The great advantage of porous materials (soil, starch, charcoal, etc.) over smooth surfaces may be due to the very rapid and complete dry- ing in the porous material and possibly to the power of absorbing gases of all kinds. Recently, attention has been called to another example of considerable importance, namely, the difference of development of bacteria in soil and in solution. The processes of ammonia and nitrate formation do not run parallel in solution and in soil; this is not due to certain chemical com- pounds in the soil, since the result remains the same if the soil is sub- stituted by the insoluble quartz sand; quartz has no absorptive powers, so this cannot account for the difference. The most probable explanation is the enormously increased surface of the water surrounding the soil particles. The surface exposed to oxygen is many times larger in a soil of a normal water content than in the same amount of water in a flask. In agreement with this explanation, nitrification, as a strict oxidation process, is greatly increased in soils with moderate moisture and is checked if the soil is saturated with water. Ammonia formation is usually favored in well-aerated soils, but occasionally it is decreased. This is probably due to the different types of ammonia-producers, some of them growing better with air, others growing better without it. Details will be given in the division on Microbiology of Soil. "167 CHAPTER VI. INFLUENCE OF MECHANICAL EFFECTS. PRESSURE. -The resistance of microorganisms to mechanical pressures is very great. Pressures of 3,000 atmospheres* will not kill the majority of bacteria in four hours. They are, however, weakened and some species will die. A specific difference between the molds, yeasts, and bacteria in this particular does not seem to exist. Of the organisms exposed to 2,000 atmospheres for ninety-six hours, Bad. anthracis, Bad. pseudodiphtherice, M. pyo genes var. aureus, Oidium ladis and Saccharomyces cerevisice survived, while seven other organisms lost the power of multiplication. Some of these were not dead, however, since they retained their motility for several days. It is noteworthy that high pressure will destroy one quality (multiplication) and not affect another (motility). Pigment-production and virulence of pathogenic bacteria were either diminished or lost com- pletely. The resistance against high pressure is necessary for the organisms which cause the decay of organic matter at the bottom of the oceans. Vertebrates breathe oxygen in the form of gas or have at least an organ filled with gas (fish bladder) ; the volume of gas is changed considerably by slight changes of pressure; this will affect organisms depending on gas. Microorganisms do not require gas as such. They can absorb gases only in solution. A change of pressure therefore will not cause a change of volume, since liquids have a very small coefficient of compression. The situation is entirely different if the liquid is not exposed to the pressure directly, but to compressed gas. In this case, the chemical effect of the gas is the deciding agent. The higher the pressure, the more gas will be dissolved in the culture medium. The fatal pressure under these conditions will vary as much as the fatal dose of an antiseptic ; it depends upon the chemical qualities of the gas, upon the pressure (concentration) , upon the temperature, and upon the organism. Some data have been given already in the chapter on oxygen require- * One atmosphere is i kg. pressure per square centimeter (or about 15 pounds per square inch). 1 68 INFLUENCE OF MECHANICAL EFFECTS. 169 ments. It was mentioned in that connection that Bact. butyricum cannot tolerate more than 0.65 per cent of the total oxygen^o.2 atm.); content in air in other words, an oxygen pressure higher than 0.0013 at- mospheres will kill the organism. The maximum pressure for B. prodigiosus was found to be about 5.4 to 6.3 atmospheres. Very few experiments have been made with other gases. Carbon dioxide at a pressure of 50 atmospheres retards the growth of bacteria in water and will sterilize it in twenty-four hours. Suspensions of pure cultures of B. lyphosus and Msp. comma are killed by 50 atmospheres carbon dioxide pressure in three hours. Milk cannot be sterilized by this pressure but bacteria do not multiply. Carbonated milk has been recommended as a refreshing drink by several investigators. The ordinary market milk will keep about two days longer under the pressure of 10 atmospheres (150 pounds) than without pressure. If pasteurized it is said to keep for a week. GRAVITY. Gravity would have a great influence upon the growth of microorganisms in liquids if their specific gravity were much greater than that of water. This does not seem to be the case however. It has been estimated by accurate weighing to vary between 1.038 and 1.065. Very much higher results (1.3 to 1.5) have been obtained by centrifuging bac- teria in salt solutions of varying specific gravity, but these data are not exact since the salt solution will diffuse into the cells and thus increase their weight. The specific gravity being very nearly that of the culture medium, it is plainly seen that gravity has but little influence. The microorganisms will live suspended in the liquid and sediment out very slowly. The slightest current in the liquid will carry them around and distribute them through the medium. The motility is of minor importance; the actual distance covered by motile bacteria has been measured, and under the most careful exclusion of currents in the liquid has been found to be about a millimeter in a minute for B. subtilis. This is very slow compared with the speed of the circulating water moved by changes of temperature or other incidental agents. Yeast cells and other gas producers use the carbon dioxide as a vehicle. The gas bubbling up in the fermenting liquid keeps it constantly in motion and moves the yeast cells against gravity toward the surface where the gas escapes and lets the cells fall back to the bottom. The production of scums and pellicles on the surface by organisms, which are heavier than the liquid they float on, is often accomplished by 170 PHYSICAL INFLUENCES. small gas bubbles between the cells. In other instances, it may be just the floating of cells having oily surfaces. The growth is influenced by gravity very little. The sporangia of molds are the only exception, growing decidedly away from the center of gravity (negative geotropism). AGITATION. For the majority of microorganisms, the quiet, undis- turbed growth of the laboratory culture is the normal or the ideal one. Such cultures, if shaken for a considerable time, show a decrease of living organisms, and it is possible to sterilize cultures by continued shaking. The effect it not a simple mechanical breaking or tearing of the cells. The bacteria break up into the finest particles. This is also the case if cultures are exposed for several days to the trembling motion caused by the working of very heavy machines. There is no grinding or tearing effect but the cells break to pieces just the same. A slight and slow agitation seems to be advantageous for many cul- tures, only continuous heavy motion proves harmful. Different organisms show wide variations in their resistance to agitation. DIVISION III. CHEMICAL INFLUENCES. CHAPTER I. STIMULATION OF GROWTH. The influence of chemical substances upon microorganisms may be helpful or harmful, or not noticeable. As helpful must be considered above all the food compounds. Unless given in such large doses as to cause a physical or osmotic effect (see chapter I, page 147) they will stimulate the development. Other substances too, which are not food, can also act as stimulants. It is a recognized fact of long standing that many poisons in very small doses will stimulate. This applies to the msot highly developed animals and plants as well as to microorganisms. Raulin noticed in 1869 that Aspergillus niger grew very much better in a nutrient solution if a small amount of zinc salt was added. He considered the zinc, therefore, as a necessary constit- uent of the mold cells. Alcoholic fermentation can be stimulated by metallic salts. It is believed by some physiologists that, as a law of nature, every substance that is injurious in a certain concentration is a stimulant in a lower concentration. A similar action of certain chemical compounds upon enzymes has been noticed, retarding in high concentrations, FlG 55 _chemo- stimulating in weaker solution. An explanation for taxis. (After Fischer.) these facts cannot be given at the present time. CHEMOTROPISM AND CHEMOTAXIS. Microorganisms manifest their preference for certain foods not by a stimulated growth alone. They also make efforts to obtain better food by growing or moving toward it, which is not a manifestation of a rudimentary intellect. Such reactions of micro- organisms, may be accounted for largely by chemical or osmotic forces. 171 172 CHEMICAL INFLUENCES. In a solid medium the hyphae of molds will grow toward the best source of food supply. This growth on account of chemical stimulation is called chemotropism, analogous to the phototropism or growth toward light. If some injurious compound is offered, the hyphae will grow away from it. Thus we have to distinguish between positive and negative chemotropism. The motile organisms, bacteria as well as protozoa, demonstrate their preference for certain food compounds by swimming toward them. This is called chemotaxis (Fig. 55). Here also a positive and negative chemotaxis must be distinguished, the latter taking place if injurious substances are present. These reactions do not seem to be of much im- portance in the life of microorganisms. CHAPTER II. INHIBITION OF GROWTH. POISONS, GERMICIDES, DISINFECTANTS, ANTISEPTICS, PRESERVA- TIVES. A great number of inorganic and organic bodies will destroy life in comparatively weak solutions. These substances are called poisons if they are considered in their effect upon man and animals. In their application to microorganisms they are generally called germicides (germ- killers), or disinfectants if the emphasis is laid upon the prevention of infection rather than upon the actual killing of the microorganisms. Analogous to the general term germicides, the terms bactericide and fungicide are used occasionally. The term antiseptic means a prevention of sepsis which may be accomplished by checking the growth without necessarily killing all microorganisms. The meaning of the word pre- servative is practically the same, only the latter is used more commonly in relation to foods, feeding stuffs and preparations of similar origin while the word antiseptic is largely used in relation to microbial diseases. A strict line cannot be drawn between any of these definitions. A disin- fectant, if diluted, becomes an antiseptic. A strong salt solution is an antiseptic for some organisms and a disinfectant for others. Of the above expressions, germicide is the most definite, but is not so commonly used as the others. MODE OF ACTION. The action of a poison upon the cell is generally considered an action upon the protoplasm. The poison is supposed to combine chemically with the cell plasma producing compounds which interfere with the continuation of the life processes and thus cause death. If the cell has been subjected to the action of the poison only a short time, it can be saved by removing the poison. Bacteria can be treated with mercuric chloride (HgCl 2 ) so that they will no longer develop if trans- ferred to a fresh medium. If the mercuric chloride is removed from the cell by means of hydrogen sulphide, some of the organisms may be revived. The action of a disinfectant upon a suspension of bacteria is not uni- form. The largest percentage of cells will be killed in a short time, 173 174 CHEMICAL INFLUENCES. \vhile a few will remain resistant for a considerable length of time. This is the case with all disinfectants. The disinfecting process resembles in many ways a slow chemical process, as the inversion of cane sugar. In the beginning, the reaction is very rapid, because plenty of the cane sugar is present; after a certain time, the action is much slower, because 3500 3000 Z500 9,000 I 500 1000 500 \ \ 0\ i f _A 10 20 30 HO 5-0 FIG. 56. Curve of disinfection. Spores of Bact. anthracis in mercuric chloride solu- tion. (After Chick.) most of the sugar is decomposed; finally it seems to nearly cease. It is the same with disinfection; at first many bacteria are present, but they are killed rapidly and only a few are left. These few die much more slowly than the first ones, not because they were more resistant, but simply as a consequence of the chemical law that the less there is of the react- ing substances the slower is the rate of reaction. The curves in INHIBITION OF GROWTH. 175 figure 56 show the numbers of living spores of Bad. anthracis suspended in mercuric chloride solution. The continuous solid curve gives the result in a o . 2 1 per cent solution, the dotted curve indicates a o . 1 1 per cent solution. The number decreases rapidly in the first few minutes, but the rate of dying is not constant, and even after a comparatively long time, a few spores remain alive. Similar curves are obtained in the destruction of microorganisms by heat, by drying and by freezing. FACTORS INFLUENCING DISINFECTION. The efficiency of a disin- fectant depends upon several factors. Moisture is necessary a dry poison has only a very slow action upon microorganisms. For this reason, absolute alcohol has not nearly the same germicidal power upon dry bacteria as diluted alcohol; the strongest poisonous effect is obtained by a 40 to 50 per cent solution; bacteria suspended in water die the more quickly the stronger the alcohol. The necessity of moisture is further demonstrated in the sterilization with gases, as with formaldehyde. The effect of formaldehyde gas without the provision of a very moist atmos- phere is surprisingly weak. The temperature is also quite an important factor in the study of dis- infectants. Since poisoning is supposed to be a chemical effect, it must be expected that the poisoning process like other chemical processes will take place faster at a higher temperature. This is actually the case. It is possible to cool a disinfectant solution to the extent that it is only an antiseptic. On the other hand, it is easily seen that above the optimum temperature, where the growth is not very vigorous, and when the dis- infecting power of the poison is increased considerably by the higher temperature, a very small amount of poison will have a very strong germi- cidal effect. The combination of high temperatures with a disinfectant has been suggested as a means of sterilizing foods. This has been tried in the case of milk with hydrogen peroxide at 50 to 60. It makes a considerable difference whether the organisms which are tested with a certain disinfectant are in a culture with their food material, or suspended in water or salt solution without any food. It is very pro- bable that part of the disinfectant is acted upon by the food products which are partly protein substances and are in many ways similar to the protoplasm of the bacterial cells. It is especially difficult to poison bacteria in blood, pus, or similar material. The sensibility of microorganisms in pure water is remarkable. Very small doses which would not be 176 CHEMICAL INFLUENCES. considered efficient under any other condition, will destroy microorganisms in pure water. The age of trie culture and the stage of development will naturally change the resistance of a species materially. The old cultures which are past the culmination of growth will be much more sensitive to any poison unless a spore-producing organism is under test. In this case, we find a greatly increased resistance, similar to the increased resistance of spores against drying and heat. THE CLASSIFICATION OF DISINFECTANTS is very difficult as long as we cannot explain completely the process of poisoning. It is impossible to arrange them according to the intensity of action, because the intensity of influence depends not only upon the disinfectant, but also upon the species of organisms. Some yeasts can resist ten times as much alcohol as certain bacteria. Formaldehyde is not nearly as strong an agent with molds as it is with bacteria. The disinfectant concentration of a poisonous substance is not absolute. The simplest method of grouping is by chemical structure and qualities. Of the following natural groups can be distinguished acids (inorganic and organic), metallic salts, hydro- carbons (aliphatic and cyclic), alcohols (aliphatic and cyclic), aldehydes, anaesthetics, essential oils, oxidizing agents and reducing agents. The first three groups, acids, alkalies and salts, can be distinguished from the rest as electrolytes; the strength of acids and alkalies (chemically speaking) is measured by the degree of electrolytic dissociation. The disinfectant value follows largely the same law. The strongest acids in the chemical sense are also the strongest disinfectants. There are ex- ceptions, however, where, besides the poisonous effect due to the degree of dissociation, there is a specific effect due to the chemical structure, as in the case of nitrous, salicylic and hydrocyanic acids. The same is true of alkalies. With metallic salts, the action will depend mainly upon the metal in solution, but the electrolytic dissociation is also of importance. NaCl will decrease the dissociation of mercuric chloride (HgCl 2 ) and de- crease also its disinfectant power. Mercuric chloride dissolved in abso- lute alcohol is not dissociated. In this case, it has almost no action upon bacteria. Acids are not commonly used as disinfectants, except in the household, but they play a certain role in nature The common fruits contain so much acid that bacteria cannot easily attack them; the decaying of fruit is almost exclusively due to molds which have a preference for acid media; INHIBITION OF GROWTH. 177 yeasts, too, are quite resistant to acid and can become accustomed to quite strong acids; it is customary in the manufacture of industrial alcohol from potatoes to prevent bacterial growth by adding about i per cent of lactic acid or very active lactic bacteria together with an acid-tolerant yeast, bred especially for this purpose. The acid in the stomach of man and animals plays an important role as a sterilizing agent for the food. Many microorganisms are killed in the stomach. In the household, the natural acidity of fruit helps in keeping canned fruit, preserves and jellies. Especially in heating, the acid together with the high temperature has a very strong germicidal effect. Vinegar is often used to preserve fruit and vegetables; in some parts of the country, meat is kept in butter- milk. Benzoic and salicylic acids are often used in the preservation of fruit and vegetables. Their poisonous influence is not so much due to the acid reaction but to the specific chemical character of these compounds. Of the alkalies, only one is used extensively, namely, lime; quick-lime (CaO) is considered a valuable disinfectant for excreta in privy vaults; it is universally applied as a white-wash in stables, barns, poultry houses and similar buildings. Quite commonly, it is used as "milk of lime" (one part of slaked lime with four parts of water). It should be kept in mind that the calcium oxide unites with the carbon dioxide of the air and thus gradually loses its disinfecting power. Of the metallic salts, many are well-known germicides. The most powerful disinfectant is mercuric chloride (HgCl 2 ) which is one of the standard disinfectants. It is generally used in a dilution 1:1000 which is sufficient to kill all vegetative cells as well as spores in a few minutes. Quite commonly, hydrochloric acid or salt is added, to prevent coagula- tion or precipitation of slimy or albuminous matter which would protect the enclosed bacteria from immediate contact with the poison. The addition of hydrochloric acid or any chloride decreases somewhat the disinfectant value for bacteria suspended in distilled water because it decreases the electrolytic dissociation. Another disinfectant of remarkable strength is silver nitrate; it is not used commonly because of its high price. It also decomposes easily and leaves dark spots on the skin and clothes. Of the other metallic salts copper and iron sulphate are not used extensively, though recommended for the disinfection of feces. Zinc sulphate may be applied to mucous membrane the same as silver nitrate. Many other salts may be used 12 178 CHEMICAL INFLUENCES. occasionally for disinfecting purposes, though the expense or undesirable qualities prevent their common application. The alcohols are well known for their poisonous effects, but the value of ethyl alcohol as a disinfectant is usually overestimated. It takes quite strong alcoholic solutions, more than 20 per cent, to kill certain yeasts and the spores of some bacteria hi less than a day, and a complete sterilization by alcohol hi a few minutes cannot always be guaranteed even with 50 to 60 per cent solution. It has already been mentioned that desiccated organisms are very resistant to concentrated alcohol, more so than to a 50 per cent mixture. Methyl alcohol is weaker, the higher alcohols, es- pecially amyl alcohol, are stronger disinfectants than ethyl alcohol. They all give good results hi the presence of water while the absolute alcohols have scarcely any effect upon desiccated bacteria. None of these alco- hols in whatever concentration they may be used, can be relied upon to kill bacterial spores. Stronger germicidal effects can be obtained by the alcohols of the benzene group, of which phenol or so-called carbolic acid (C 6 H 5 OH) is the simplest representative. Phenol, like ethyl alcohol, is not as effective as is commonly believed. It is applied in solutions from 0.5 per cent to 5 per cent ordinarily, but it usually takes a long time even for the 5 per cent solution to kill vegetative cells as Bact. tuberculosis or B. coli; it is inefficient against anthrax spores. More powerful are the higher cyclic alcohols, of which the cresols are examples. They are used extensively as disinfectants and antiseptics. They are, together with phenol, coal-tar constituents and are sold commercially under many different names, either pure or mixed with soap or other disinfectants which make them emulsify readily in water. The cresols are almost insoluble in water, and not as effective in solutions as they are in emulsions. The disinfecting properties of tar come from the cresol contained in it. Hydrocarbons are used only for laboratory experiments as very weak antiseptics. The aliphatic bodies, as methane, etc., which constitute a large part of coal gas, have but very little effect upon bacteria; the gas is used occasionally in place of hydrogen for growing anaerobic bacteria. Benzol, xylol, and toluol are antiseptics, if shaken frequently with the liquid to be protected, but they are not reliable as disinfectants. The same is true with the common anaesthetics, ether and chloroform. The high prices of these agents forbid their general use, but they are sometimes used for laboratory work. INHIBITION OF GROWTH. 179 The essential oils have a little more practical importance. Some of these are the main constituents of mouth washes, especially the oil of pepper- mint (menthol) , of thyme (thymol) , and of eucalyptus (eucalyptol) . Their action is very weak, however. The volatile oils of spices have to be con- sidered in the preserving of fruit, pickles, catsups, and other food products. Though the antiseptic value in general is insignificant, certain micro- organisms are sensitive to certain spices. The bacteria of the mesen- tericus group are said to be suppressed entirely by quite small quantities of garlic, while others, like the lactic bacteria, are not affected at all. Cloves, cinnamon and alspice are the most efficient spices, while the disinfectant power of black and white pepper, and mustard is very small. The most important disinfectant has not been mentioned, because it does not belong to any of the above groups. This is formaldehyde. Formaldehyde (HCOH) is a gas, soluble in water to the amount of 40 per cent at room temperature; it does not attack metal, clothing, wood- work, and is, therefore, preferable to many other disinfectants for steriliz- ing rooms. It kills spores of bacteria in a short time in a 1:1000 di- lution. Its greatest importance lies, however, in its gaseous nature, because it can be applied to rooms and buildings by simply evaporating it. The saturated 40 per cent solution can be evaporated directly or by generating steam which passes through the formaldehyde solution; this latter method has the advantage of saturating the air with moisture, which increases the power of the formaldehyde gas. Formaldehyde can also be obtained in a dry form; it polymerizes to a white crystalline substance, paraformaldehyde ((HCOH) 3 ) which can be changed back to formaldehyde gas by gentle heating. This paraformaldehyde is com- monly used instead of the liquid, because it is more easily handled and is quite inoffensive in its solid form, while the formaldehyde solution has a very penetrating odor and is exceedingly harmful to the mucous mem- brane of the respiratory organs. Of the oxidizing agents, oxygen itself has already been mentioned. Though it is able to destroy certain anaerobic bacteria, it cannot be called a disinfectant. For this purpose, oxygen must be activated; such oxygen can be obtained in the form of ozone (O 3 ). It is formed in air under the influence of electric discharges and can be produced at a price low enough to allow its application for use in the sterilization of water. It has also been recommended for preservation of milk. Hydrogen peroxide (H 2 O 2 ) resembles ozone in its chemical reactions; l8o CHEMICAL INFLUENCES. it changes readily to H 3 O+ O, and this oxygen atom in the nascent state is quite effective as an oxidizing agent. For an antiseptic, it must be used in at least a i per cent solution, and for an absolutely reliable disinfectant a still higher concentration is required. It loses its disinfecting property easily because it is decomposed readily by the peroxidases of tissues and organic liquids as blood, milk and pus. It is used in the preservation of milk. Hydrogen peroxide is slowly decomposed by the katalase of milk thus disappearing completely. Chlorine in its gaseous form is not used as a disinfectant, though its germicidal power is quite strong. The so-called "chloride of lime," manufactured by absorbing chlorine in slaked lime, gives in water hypochlorite and free chlorine; these substances are good germicides and chloride of lime is used in the disinfection of privy vaults, and other places in which it may be employed without injury. Potassium permanganate is only incidentally used as a disinfectant. Its chemical qualities prevent an ordinary use. Sulphurous acid, or sulphur dioxide (SO 2 ) was for a long time a standard disinfectant and is still used occasionally for fumigating rooms, stables, barns and out-buildings though it is substituted more and more by formaldehyde which can be applied almost as easily. The burning of sulphur is an extremely simple process, but it requires a moist air to dis- infect properly, and under these circumstances it will attack metal, dyes of clothing and even the fiber itself. DIVISION IV. MUTUAL INFLUENCES. INTRODUCTION. The biological relations of microorganisms are of the greatest im- portance in nature. Pure cultures in nature are very rare and of exceptional occurrence; they are hardly ever found except in certain diseases of man, animals and plants. Generally, nature works with mixed cultures. All natural fermentations, decompositions and putrefractions are accom- plished by a number of different species among which perhaps one domi- nates, but is influenced by the rest. The study of the mutual relations of microorganisms is in the very first stage as yet; practically all laboratory work is done with pure cultures. The experiences obtained with pure cultures are not sufficient to explain all microbial activity in nature. There are many possibilities of mutual influence between different organisms. Generally three main cases are distinguished: symbiosis, where two organisms profit by the combination; melabiosis, where one profits by the other's action without benefiting the other in return, and antibiosis, where one organism injures the other. These cases cannot be separated strictly. The relations are not always constant through the entire development of the cultures; an originally beneficial influence may change to an injurious one in a few days. Many terms have been coined to designate all these various possibilities, but in order to avoid this multiplicity of more or less indefinite names for the various relations, the general term "association" has come into use, especially when the relationship is not well understood. SYMBIOSIS. Symbiosis is not very common among microorganisms, and it is difficult to find examples where true symbiosis exists through the entire development of both organisms. The association of lactic bacteria and Oidium lactis in milk is, for a certain period at least, a symbiosis. The 181 l82 MUTUAL INFLUENCES. bacterium will produce only a certain amount of acid, and then it can grow no more because the acid is too strong; the mold will destroy the acid and thus gives the bacterium a chance for continued activity. The bacterium produces the acid which the mold likes; the mold in turn removes the excess acid which otherwise would check the bacterial activity. True symbiosis is more common in the relation of microorganisms with higher plants and animals. The standard example in the plant kingdom is Ps. radicicola in the nodules of legumes, feeding on carbohydrates pro- vided by the plant and furnishing the plant nitrogen from the air which the plant cannot assimilate directly. The typical example in the animal kingdom is B. coli in the intestine of animals, being nourished by the food of the animal and rendering the food more easily digestible. METABIOSIS. Metabiosis may be considered a one-sided symbiosis; two organisms live together, but only one is benefited the other remains uninfluenced or later may be injured by the association; the latter case is the most common. In this relation, one usually prepares the food for the other. It has pre- viously been mentioned that the metabolic products of one species serve as food for another species, thus breaking up the various organic compounds step by step to smaller and simpler molecules. Quite commonly, each step is accomplished by a different species of microorganism. Conse- quently, metabiosis is a very common occurrence among microorganisms. The classical example is the two nitrifying bacteria: the nitrate bac- terium is unable to oxidize ammonia, and depends entirely upon the ni- trite bacterium to oxidize the ammonia to nitrite; then, and only then, can the nitrate bacterium grow. The relation between yeasts and acetic bacteria is also very well known. The yeast ferments the sugar to alcohol, and then the acetic organisms oxidize the alcohol to acetic acid. The yeast is in no way helped by the acetic bacteria, while these could not form acetic acid from sugar readily. These bacteria depend upon the action of the alcohol-forming yeast. Other cases of metabiosis are found in the association of lactic bacteria with certain protein destroying organisms. The lactic bacteria often develop much better if the protein bacteria grow together with them or have grown previously in milk. Metabiosis does not require the growth INTRODUCTION. 183 of the two associated organisms at the same time. The effect will be the same if first the one and later the other develops, and even after the first organism is killed or removed, its effect upon the pure culture of the second will still be noticed. This does not occur in the case of symbiosis. One species can favor the development of another by other means than food provision or preparation. Certain bacteria cannot live in acid media, and molds or Mycodermce destroying the acid will render possible the growth of these bacteria though they do not provide them with food. This is the case in the ripening of certain soft cheeses. Another example is the production of heat by fermenting organisms in manure, hay, ensilage, enabling the development of thermophile organisms. A very interesting and important problem is the growth of strictly anaerobic bacteria near the surface of liquids in association with some aerobic bacteria. How this is really possible cannot be satisfactorily explained. Though the aerobic bacteria continuously remove the oxygen from the water a certain amount will remain, sufficient to prevent the growth of the anaerobic bac- teria under ordinary conditions. There seems to be a certain protective influence derived from the aerobic bacteria, the nature of which is un- known. ANTIBIOSIS. The standard examples of antibiosis are the alcohol production by yeast in sugar solutions and the acid production by lactic bacteria in milk. Fresh cider contains a large number of bacteria, yeasts and molds; some of these organisms cannot develop in the acid medium, but many will be- gin to grow. Some of the bacteria will produce or destroy acid, others may begin to work on the nitrogenous material of the cider, and the yeasts produce alcohol and carbon dioxide. The carbon dioxide will soon satu- rate the cider and begin to bubble up, thus removing the other gases. The molds will stop growing if the oxygen is taken away, but some of the bacteria may continue growing until the alcohol concentration checks their further development. They first cease to grow, then cease to produce acid and finally die, while the yeast is still continuing in the fermentation. In the lactic fermentation of milk, Bact. lactis acidi combats all other organisms by a rapid production of lactic acid. Though it is present in fresh milk only in very small numbers, its rapid growth and the forma- tion of acid which will check and even kill most other bacteria soon makes it the dominant organism in the flora of milk, and at the time of curdling, 184 MUTUAL INFLUENCES. it is often difficult to find any other organisms besides the lactic bacteria. In the preceding chapter was mentioned the metabiosis of certain protein- digesting bacteria with Bad. lactis acidi. This metabiosis can be con- sidered as such only from the standpoint of the lactic organism. The protein bacterium is killed by the acid formed by the rapidly growing lactic bacteria. From the viewpoint of the protein bacteria, the relation is antibiosis. Another illustration of antibiosis is the acetic fermentation. The formation of acetic acid prevents the development of all bacteria and of most yeasts and molds. In all these cases, the deciding agent is a well-known chemical com- pound. In other combinations, the principle is unknown. Bad lactis acidi will check the growth of B. subtilis not only in milk where it forms acid, but also in sugar-free broth where acid production is impossible. Acetic bacteria act upon the yeast cells not only by means of the acetic acid pro- duced, but also by some other, unknown agent, since vinegar is more injurious than the corresponding amount of pure acetic acid in water. A very remarkable organism is Ps. pyocyanea; it secretes a substance, pyocyanase, which will kill and dissolve the cells of other bacteria rapidly. Parasitism, which would be classified under antibiosis, has not been found to exist among bacteria or yeasts; but we know of cases where one mold grows on the other; this is especially true with the largest represen- tatives of the mucor family, which are often attacked and sometimes killed by smaller fungi. PART III. APPLIED MICROBIOLOGY. DIVISION I* MICROBIOLOGY OF AIR CHAPTER I. THE MICROORGANISMS OF THE AIR AND THEIR DISTRIBUTION. The atmosphere is not the normal habitat of bacteria, for growth and multiplication cannot take place in it under ordinary conditions. The phrase "microorganisms of the air" is therefore somewhat ambiguous. The small size of microorganisms enables them to remain suspended for considerable periods when physical forces have separated them from the substrata on which they have developed. MICROORGANISMS PRESENT IN THE AIR. Molds, bacteria, and yeasts are all found in the air under certain conditions. The first two are usually relatively abundant, the latter are less common. The common molds have adapted themselves for the most part to wind distribution. They bear spores that are small in size and with a surface that is not readily moistened. These spores are resistant to desiccation and light and remain viable for a considerable time even under unfavorable conditions. Furthermore, the fruiting bodies of many, though not all molds, show a distinct negative hydrotropism, i.e., the mycelium remains in contact with the moist substratum while the threads which bear the spores rise at right angles to it. These latter are so sensi- tive that they can detect slight differences in the moisture content of the air and grow in the direction which will bring the spores into the driest * Prepared by R. E. Buchanan. l86 MICROBIOLOGY OF AIR. situations. A slight current of air will detach the spores from these structures and carry them long distances. Bacteria and yeasts lack the specific adaptations for wind distribution found in molds. The material upon which they have been growing must be dried and pulverized before they can be blown about. Many species produce spores or other resistant cells, and physiologically, are as well adapted for air distribution as are the molds. OCCURRENCE IN THE AIR. Microorganisms are found free in the air, attached to particles of dust, or enclosed in minute drops of water. Mold spores are commonly free or in unattached clusters. Bacteria and yeasts are usually associated with dust particles, frequently the pulverized sub- stratum on which they have been growing. Not all dust particles have living organisms attached. It has been computed that in the air of London during a fog there is only one living organism for over thirty-eight millions of dust particles. Microorganisms are sometimes sprayed into the air with water. Droplets containing bacteria are thrown off in the saliva in coughing or in speaking, and from the surface of fermenting liquids on which bubbles are bursting. When the drop is small enough, the air currents keep it in suspension and the water soon evaporates and frees the organism. This brings about the condition first discussed, free bacteria in the air. The decrease in weight and size incident to this loss of water probably accounts for the fact that the so-called "infectious droplets" are sometimes carried for considerable distances. How MICROORGANISMS ENTER THE AIR. In comparatively few in- stances do microorganisms possess mechanical devices for projecting the spores or other cells into the air for wind distribution. Usually the or- ganism is passive and is freed only by air currents or by mechanical agitation. Some molds, as has been stated, release their spores even in the presence of moisture, so that complete desiccation is unnecessary for their dispersal. Bacteria and yeasts, on the other hand, are not usually given off from moist surfaces. Only when dry and pulverized can the bacterial medium be readily blown about. Hansen found that in the im- mediate vicinity of a heap of decaying malt, the air was comparatively free from bacteria. Winslow has shown that sewer air is frequently practically free from bacteria although the surface with which it comes in contact teems with bacterial life. Mechanical agitation often throws large numbers of organisms into the air. Moving hay and straw, groom- ing animals, sweeping a floor or carpet will multiply the dust and bacterial MICROORGANISMS OF THE AIR. 187 content of the air many times. In a similar manner, tiny germ-holding droplets may be scattered by the splashing of sewage or of fermenting or putrefying liquids, and in speaking, sneezing or coughing. CONDITIONS FOR SUBSIDENCE OF BACTERIA. The length of time during which an organism may remain suspended in the air is dependent upon several factors. Small particles settle out more slowly than large for the reason that as the size of an object is decreased, the surface area decreases less rapidly proportionately than the volume. The lifting effect of air currents depends upon the ratio of surface area to volume and specific gravity. The smaller the object, therefore, the greater is the resistance to subsidence. Consequently, bacteria usually settle out of air very slowly if free in a quiet atmosphere. The time of suspension is determined also by the velocity of the air currents. While considerable velocity may be necessary to dislodge microorganisms and bring them into suspension, a very slight air current will sustain them. Winslow has found that a current of seventeen inches per minute is sufficient to sustain B. prodigiosus. The relative humidity of the air is also an im- portant factor. In a supersaturated air solid particles, such as bacteria, become nuclei of condensation for water and quickly settle out. When dust is present in considerable quantities, and certain electrical or mois- ture conditions exist, flocculation occurs and the larger bodies so formed subside rapidly. The character and abundance of surfaces with which the suspended particles may come in contact also play an important part. Moist surfaces are much more effective in retaining particles than those which are dry. DETERMINATION OF THE NUMBER OF BACTERIA IN THE AIR. The number of bacteria in the air is frequently determined by exposing open petri dishes of gelatin or agar in different places for definite periods. This is a comparative quantitative method only. The number of colonies developing upon these plates will give the number of dust particles having living spores or cells upon them that fall in the given area under the con- ditions of the experiment. Evidently this is of value only for rough comparative work as constantly shifting currents of air usually intro- duce great errors. A somewhat more accurate method is to draw meas- ured volumes of air into a flask, the bottom of which is covered with a layer of gelatin or agar. The colonies which develop represent the number of organisms which settle out from the given volume. More accurate results still may be obtained by drawing measured volumes of 1 88 MICROBIOLOGY OF AIR. air in small bubbles through liquid gelatin. Practically all of the particles will be retained and the number of colonies which develop may be counted. This method is sometimes modified by drawing the air through a definite volume of water, care being taken to insure sufficient contact of air and water to remove all dust particles. A proportionate part of the water is then plated and the number of organisms estimated. Air is sometimes drawn through a filter made of sugar, sodium sulphate, or sodium chloride, and this material then dissolved in water and plated. Sand, asbestos, glass, etc., are sometimes used as air filters, then thoroughly washed, and the wash water plated. Relative quantitative examination of the air is of more historical than practical importance. It has been useful in the development of the germ theories of fermentation and of disease and in overthrowing the theory of spontaneous generation. There is so little ordinarily to be learned by a study of the air flora that a comparison of plates exposed directly will usually suffice. Where more accurate results are desired, one must resort to one of the filtration methods discussed above. Qualitative determinations of the species of air organisms are not often made. When necessary it may be done by simple examination of the colonies developed on the plates or by animal inoculations made from the water used in the air filter. It is sometimes necessary to vary the composition of the medium used in order to favor the development of certain types of organisms desired, for example, a higher percentage of molds will be found and a more luxuriant development will take place if wort agar or acid gelatin is used. NUMBER OF BACTERIA IN THE AIR. The number of bacteria in the air is determined by a variety of conditions. The velocity of air currents and the nature of the surface with which these currents will come in con- tact, are probably most important. Bacteria are usually more abundant on quiet days in the air of buildings than out of doors, but on windy days the reverse is true. They are often more abundant in cities than in the country. Fewer are found at high altitudes and over large bodies of water. Frankland found that there are fewer in winter than in summer They are washed from the air during rains. Bright sunlight destroys many. The nature of the soil and the vegetation covering it has a marked influence. The following figures from various authors are appended to serve as an index to what may be expected in the air content of bacteria. MICROORGANISMS OF THE AIR. Locality Number of organ- isms per cubic meter 189 Observer Outdoor air, Boston 100-150 bacteria. Sedgwick and Tucker Open air 50-75 molds. 100-150 bacteria. Fischer. Open field Uffelman Seacoast . . IOO Uffelman Mountain altitude 200 meters o Pasteur. Mont Blanc . . *. . . 4-11 Ellis. Spitzbergen (Arctic Regions) o Levin. Middle of Paris 4,000 Ellis. Paris Street . . Fischer. Tailor's Room in Whitechapel 17,000 Ellis. Boot Workshop 2? .OOO Ellis. SPECIES OF ORGANISMS IN THE AIR. Penicillium is the most common mold isolated from the air. Next in importance are Mucor, RJiizopus, and Aspergillus in the order given. In addition to these a considerable number of species of hyphomycetous molds are occasionally found. TorulcB, but not true yeasts, are usually common. Bacteria are either spore-bearing soil bacilli or cocci. Of the former, B. subtilis, B. mycoides, and related forms are ubiquitous. Sarcina lutea and Sarcina aurantiaca and certain other chromogenic cocci are to be found in almost every plate exposed. Since the air does not have a true flora, the species as well as the number of bacteria present must depend entirely upon the character of the environment. CHAPTER II. MICROBIAL AIR INFLUENCE IN FERMENTATION, DISEASES, ETC. AIR AS A CARRIER OF CONTAGION. There are many popular mis- conceptions of the influence of air upon health. Experience early taught that exposure to the night air in certain localities or to swamp air during certain seasons was generally followed by disease. Naturally, the air itself was held responsible. We know now that certain fevers, malaria, etc., are caused in every instance by infection with specific microorganisms and that these organisms are not usually carried by the air but by insects, such as the mosquito, in water and food. Nor can the emanations from decaying organic matter or sewer gas itself be held to produce disease directly. Before the establishment of the germ theory of disease, leading sanitarians held that sickness was induced by the gases from decaying organic matter, by the effluvia from cess-pools and by sewer gas. However important the places named may be in harboring disease microorganisms, we have learned that the air itself rarely acts as a carrier. Sewer gas has been shown to be unusually free from bacteria. Hazen says, "After many years of experience and long continued investigation, there is not the slightest reason to believe that infectious diseases are carried by the air of sewers." Undoubtedly the air does play some part in the carrying of disease germs. In certain diseases, as the exanthemata (smallpox, measles, etc.), the infecting agent may be present on the dry skin and may be blown about and inhaled. This means, however, is not established. In certain nasal, tracheal, and pulmonary infections, the organisms may be spread through speaking, sneezing, and coughing, for the infec- tious droplets, as has been seen, remain suspended for a time in the air. Pyogenic cocci are present in the mouth and care must be used in surgical operations that the mouth is so protected that none of these organ- isms gain entrance to wounds. Rarely, if ever, are intestinal infections, as typhoid or cholera, spread through the air. We may therefore con- clude that air is of secondary importance as a carrier of infection. It 190 MICROBIAL AIR INFLUENCE IN FERMENTATION, DISEASES, ETC. 19! may be of importance in a crowded work-room, but even under these con- ditions it is probable that transmission of infection comes about more frequently through actual contact or through food and drink. ORGANISMS or THE AIR AND FERMENTATIONS. A uniform inoculation with soil bacteria such as produce the nodules on the roots of legumes is obtained over considerable areas through the action of the wind in blowing dust particles. The bacterial flora of milk is to some extent dependent upon air currents as is also the development of the molds necessary to the proper ripening of cheese, such as the Camembert. Acetic, butyric, and other ferments are likewise distributed in this manner. The organisms responsible for putrefaction and decay, the molding and spoiling of foods are wind-borne. FREEING AIR FROM BACTERIA. Air is most commonly freed from bacteria by sedimentation, for this is the ultimate fate of most dust par- ticles. We have seen that they gradually subside in a quiet atmosphere. When large quantities of pure air are required, dust and bacteria may be removed by passage through a spray of water or through various types of niters, such as cotton, glass, wool, etc. A familiar example of this type of filtration is the laboratory use of cotton plugs in test-tubes. It is sometimes necessary to resort to fumigation to destroy the organisms of the air when an undesirable species is present. DIVISION II. MICROBIOLOGY OF WATER AND SEWAGE. CHAPTER I.* MICROORGANISMS IN WATER.f Water is necessary in the life of man. Besides its use as a beverage, for cooking, and all domestic purposes, it is largely used in many manu- facturing industries; therefore, the study of its chemical and biological content is one of the most important features of modern hygiene. All natural waters contain microorganisms, which gain entrance from many sources. Under the influence of the sun, sea water evaporates and forms a water vapor, which we call clouds; and these, driven by the wind over the land, are precipitated as rain and in the form of snow or hail. Most of this water collects from vast areas into brooks, streams, rivers, lakes, or in subterranean streams, and finally reaches the sea whence it came. The water vapor arising from the sea or land contains no organisms; but as soon as the vapor is precipitated microorganisms find their way into it. These come from the air and from the soil. Some of them find in water sufficient nutriment for their life and growth; and, because of their constant presence and evident ability to thrive in water, they are some- times spoken of as belonging to the "water flora ." Others, such as the soil bacteria, are found only at certain seasons, as after rain or during flood- * Prepared by F. C. Harrison. f For specific details regarding methods of analysis and a fuller presentation of the subject, readers may consult any of the following excellent books: 1. Savage, W. G.: The Bacteriological Examination of "Water Supplies, London, H. K Lewis, 1906. 2. Horrocks, W H. : An Introduction to the Bacteriological Examination of Water, London, J. and H. Churchill, 1901. 3. Prescott and Winslow: Elements of Water Bacteriology, 2nd Ed. New York, Wiley & Sons, 1908. 192 MICROORGANISMS IN WATER. U)J time, and flourish only for a time; while some few, such as intestinal organisms that find their way into water, survive for only a short period. CLASSES OF BACTERIA FOUND IN WATER. The bacteria found in water are here roughly divided into: (a) natural water bacteria; (b) soil bacteria from surface washings; (c) intestinal bacteria, usually of sewage origin. But there is no strict dividing line between these three groups; for some organisms belonging to the water flora are found in the soil, and vice versa. Water draining from manured land frequently contains intestinal organisms. The division, however, is sufficient for all practical purposes. NATURAL WATER BACTERIA. The natural water bacteria are generally regarded as harmless to man. These organisms are frequently numerous in river, lake, and all surface waters; certain species predominate at one season, and disappear at another. Some of the best known are mentioned below. Several investigators have grouped the bacteria found in water into classes according to their biochemical properties. Where groups are subsequently referred to, the classification is that used by Jordan and followed by many other workers. B . fluorescens liquefaciens , Group V, together with some closely allied varieties, is probably more frequently found in water than any other form, and is easily recognized by the green fluorescence and liquefaction it pro- duces in gelatin. B. fluorescens non-liquefaciens, Group VI, as the name implies does not liquefy gelatin, but produces characteristic colonies with a fluorescent shimmer, is often very abundant in river waters, and is representative of a group comprising B.f. longus, B.f. tennis, B.f. aureus, and B.f. crassus. Certain organisms which liquefy gelatin and acidify milk classed by Jordan in his Group VIII are quite common at certain seasons. Some of these are soil organisms and are closely related to the proteus group; and some of them are B. liquefaciens, B. punctatus, B. circulans. Chromogenic bacilli and cocci (Groups XIII, and XI V] are often present in water. Of those producing red coloring matter, the well-known B. prodigiosus is the type of the group; others are B. ruber, B. indicus, B. rubescens, and B. rubefaciens. Several yellow and orange organisms are commonly found, such as B. aquatilis, B. ochraceus, B. aurantiacus, B.fulvus, etc. At certain times, particularly in river and brook waters, organisms 1 94 MICROBIOLOGY OF WATER AND SEWAGE. producing violet pigment are quite common. B. violaceus or B. janthi- nus, as it is sometimes called, is the prevailing type; others are B. lividus, B. amethystinus, and B. coeruleus. The chromogenic cocci produce either orange or yellow pigment, and as a rule are not numerous in water. Sarcina lutea is the most common species. Non-chromogenic cocci (Group XV) are more frequent. M. candi- cans, M. nivalis, M. aquatilis, are non-liquefying forms, and M . coronatus is the type of those which liquefy gelatin. SOIL BACTERIA FROM SURFACE WASHINGS. During times of flood, high water, and after rains, numerous soil organisms are found in natural waters; and occasionally certain species persist for a considerable time. Among the commonest species is B. mycoides, with its characteristic rhizoid colony; also B. sublilis, B. megatherium, and B. mesentericus vul- gatus, with its allied varieties; likewise B. m.fuscus and B. m. rubera\\ belonging to Jordan's Group VII, and having many characters in common, such as characteristic colonies, followed by liquefaction when growing in gelatin, production of spores, etc. Cladothrix dichotoma, one of the thread bacteria, easily recognized on gelatin plates by the brown halo that surrounds the colony, is often found in fresh and stagnant water, and in most soils. It seems to flourish where- ever there is much organic matter. These are the soil organisms most often found when beef peptone gel- atin is used for isolating purposes; but if other media are used, a different flora appears, and we find nitrifying organisms, yellow chromogens, etc. INTESTINAL BACTERIA, USUALLY OF SEWAGE ORIGIN. Proteus Group. -There are several groups of sewage organisms found in impure water; some of these are very abundant in crude sewage, but are not found in such relatively large numbers in contaminated water. Jordan's Group III contains the organisms belonging to the large proteus group, the principal species being B. mdgaris, B. zenkeri, B. mirabilis, B. zopfii, the sewage proteus of Houston, and B. cloaca. All these are frequently found in impure water, and in sewage. In the latter Houston has found as many as 100,000 per c.c. All these organisms are motile, liquefy gelatin, and produce gas in dextrose and saccharose broth, and little or none in lactose; reduce nitrates, curdle milk, produce indol, and give a fecal, disagreeable odor in broth or other media. Sewage Streptococci. The streptococci found in sewage are probably MICROORGANISMS IN WATER. 1 95 similar to those found elsewhere; but their appearance in contaminated water may be regarded as indicative of recent sewage contamination, because the bulk of the evidence available seems to show that they are delicate organisms, which rapidly die outside of the body. While it is easy to ascertain their presence in polluted water, it is almost impossible to enumerate them; and they do not furnish such good evidence of sewage pollution as the colon bacillus. They may be said to furnish valuable confirmatory evidence of sewage contamination. B. Enteritidis Sporogenes. This resistant, spore-bearing organism is usually present in the intestinal tract of man ; is found in sewage, milk, and dust; and occurs in foodstuffs, such as wheat, oatmeal, rice, etc. On account of its ubiquity and the resistance of its spores, it cannot be considered a good indicator of excretal pollution. B. Coli. The presence of this organism in potable water is generally accepted as the best bacterial indicator of sewage pollution. It must be remembered, however, that there are many varieties of this organism, to which certain investigators have given specific names, even when the differences from the type organism have been very slight. It may be well to mention some of these, to avoid confusion in the mind of the reader. The true colon bacillus, B. coli, or B. coli communis, or B. coli communis verus, is a short bacillus with rounded ends, motile, forms no spores and is Gram negative, does not liquefy gelatin, produces acidity and coagulation in litmus milk, gives rise to acid and gas in glucose and lactose media, causes canary-yellow fluorescence in neutral red media, and produces indol when grown in peptone water. The term "Excretal B. coli" has been suggested as a convenient designation of an organism which possesses the above characteristics. A saccharose fermenting variety of B. coli has been named B. com- munior; and we have a whole series of organisms which differ more or less in various biochemical reactions, or lack some of their positive reactions. To some of these the name "para-colon" has been given; and the name "para typhoid" has been applied to those which more closely approximate to the cultural peculiarities of the typhoid bacillus. For practical purposes in the analysis of water, these distinctions are unnecessary. Bad. lactis aerogenes, a short, thick, capsulated, non-motile bacterium related to B. coli, is also an intestinal organism, and must be regarded as an indicator of sewage pollution. ig6 MICROBIOLOGY OF WATER AND SEWAGE. B. Typhosus (page 640). Very few instances are recorded in bac- teriological literature of the direct isolation of the typhoid bacillus from infected water. The organism is not long-lived, even in pure water (eight to ten days); and when exposed to the action of sewage bacteria, its longevity is greatly diminished (not more than five to six days). A few resistant specimens may remain alive for longer periods of time. Although the typhoid bacillus has been found so infrequently in water, it is well understood at the present time that the purification of the water supply of a town or city produces a marked decrease in the number of cases and in the mortality from typhoid fever, as the following table shows: (See also Fig. 57.) Deaths from Typhoid Fever per 100,000 per Year. Place Purifica- tion by Date of change Five years before change Five years after change. Percentage of reduction Hamburg Filtration 1802 ? 47 7 8S Ztirich Filtration 1885 76 IO 87 Lawrence IVIass Filtration 1803 121 26 70 Albany N. Y Filtration 1800 IOA 28 77 Not only has such a marked improvement followed the purification of public water supplies in the case of typhoid fever, but it has been shown by statistics that "where one death from typhoid fever has been avoided by the use of better water, a certain number of deaths, probably two or three, from other causes have been avoided." In the routine examination of water, no particular effort is made to isolate this organism, owing to the difficulty of the task. The tests that the present day investigator has to satisfy are extremely thorough; and unless the suspected organism conforms to the whole of these necessary tests it cannot be accepted as true B. typhosus. Msp. Comma (page 645). The spirillum, or vibrio, of Asiatic cholera is an intestinal organism; and the disease it produces is spread largely by water. Epidemics of cholera are more easily traced to their source MICROORGANISMS IN WATER. 197 Average annual death rate from typhoid fever per 100,000 of the population. 8 16 24 32 40 48 56 64 72 80 88 96 104 112 120 DEATHS SPRIN6FIELD WILMINGTON An instructive contrast between Altona'and Hamburg before the latter filtered its water, having learnt its lesson from a sharp outbreak of cholera. A FEW SCATTERED CASES Of ALTOHA^ HAMBURG. POPULATION: 600.000 CHOLERA CASES'. 17.000 DEATHS: 8.600 ALTONA: WATER FILTERED HAMBURG: WATER. UMFILTERED FIG. 57. (After G. E. Armstrong.) 198 MICROBIOLOGY OF WATER AND SEWAGE. than those of typhoid fever, owing to the "explosive" character of the disease. At the time of the outbreak of cholera in Hamburg, in 1892, the cholera vibrios were frequently isolated from the water of the river Elbe, which was used to furnish the regular supply of the city. The adjoining city of Altona also obtained its water from the same river, after it had received some of the Hamburg sewage; yet it remained practically free from the scourge, owing to the efficiency of sand niters which were used to purify the water (Fig. 57). In times of epidemic, the organism has been isolated from rivers, wells, and reservoirs in India, a country in which the disease is endemic. THE NUMBER OF BACTERIA IN RAIN, SNOW, HAIL, ETC., AND IN WATER FROM WELLS, UPLAND SURFACE WATERS, RIVERS, AND LAKES. RAIN. The number of bacteria found in rain depends upon the month of the year and the dryness of the air. When considerable dust is present in the air, the first rain beats it back to the soil; and at such time rain water contains more organisms than usual. Rain falling in densely inhabited cities always contains more microbes than rain falling on open farm land or upland pastures. A few figures will be sufficient to illus- trate: NUMBER OF BACTERIA PER LITER or RAIN WATER. Figures for Montsouris Park, Paris, France, and the average for two years. Month Number of organisms per liter Month Number of organisms per liter January .... 8 ooo July c;,6oo February I 32O Aueust . 8,300 March 2 O2O September C77O April .... 2 1A.O October "?,22O May 2 AA.O November 3, 2 so June ... ... . 56OO December 4,^70 Yearly average 5,300 per liters per month. The average for the interior of Paris corresponds with the larger amount of dust in the air, and reaches a total of 19,000 organisms per 1. MICROORGANISMS IN WATER. With a yearly rainfall of 609. 6 mm. (24 in.), the rain washes down during the year some five million organisms to the square yard. SNOW. -The results obtained from snow are similar to those ob- tained from rain; but as a rule the numbers are larger, a result doubtless due to the larger particles of the snow flakes. One investigator has found from 334 to 463 bacteria per c.c. of snow water. On the summit of high mountains snow is practically sterile, Binot not finding a single organism in 8 c.c. of water from mountain-top snow. Water issuing from glaciers is of remarkable purity, containing only from three to eight organisms per c.c.; but the numbers are larger as the distance from the glacier increases. HAIL. Hail stones usually contain large numbers of bacteria, vary- ing from 628 to 21,000 per c.c. of water obtained from the melting hail. Fluorescing bacteria have been found in some samples; and the presence of these microorganisms suggests that surface water is sometimes carried up by storms and congealed. The presence of many molds in hail is due to contamination from the air. DEEP WELLS. Deep well water and spring water contain as a rule but few organisms, usually less than 50 per c.c. on gelatin at 20, and less than 5 per c.c. on agar plates at blood heat. In a series of tests of water taken direct from forty- three artesian wells, 152.4 M. (500 feet) deep or more, the writer has found an average of 27 per c.c. for the gelatin and 1.5 per c.c. for the agar counts. These tests have extended over a period of several years; and water from deep springs has given similar results. SHALLOW WELLS. The bacterial content of shallow wells depends greatly on their location and construction. Even in those well located and constructed, the number varies with the amount of rain fall, and is often large. In polluted wells, very high numbers of organisms are found. Sedgwick and Prescott found from 190 to 8,640 bacteria per c.c. in unpolluted wells. In the same class of wells, Savage found from 10 to 100 per c.c. by the blood-heat count, and 100 to 20,000 or more by the gelatin count. Sixty polluted wells examined by the writer gave an average gelatin count of 740 bacteria per c.c.; and thirty-eight wells which were free of contamination gave an average count of 400 per c.c. Polluted wells often give counts approximating the higher numbers 2OO MICROBIOLOGY OF WATER AND SEWAGE. mentioned above; but, of course, the character of the bacterial flora is quite different. UPLAND SURFACE WATERS. There are few bacteria in upland sur- face waters draining barren uplands. Cultivation, grazing of animals, and human habitation produce other conditions. In pure waters, 50 to 300 per c.c. by the gelatin and i to 10 by the agar count are found. RIVERS. The greatest variation in the number of bacteria exists in river waters. Many factors, such as sewage contamination, temper- ature, rain fall, vegetable debris, etc., influence the microbial population. A few figures may be given for illustration. Bacteriological Examination of Rivers at and below Large Sources of Pollution (Boyce and Co-workers}. Distance Direction Munich. River Isar Cologne, River Rhine About o 6 miles above below 35 o 387 4,786 About 2 7 miles below y>ow 13 CO3 About 6 . o miles below "Os J^O 8,764 30,4^2 About 12 . o miles . . below 4. 706 I2,46o About 15. o miles below 3 602 QCQC About 26. o miles below 7,860 In the Chicago drainage canal, Jordan found 1,245,000 bacteria per c.c. at Bridgeport; 650,000 at Lockport, twenty-nine miles below; and 3,660 at Averyville, 159 miles below. Below where the sewage of Peoria enters, the numbers rise to 758,000 at Wesley City, and decrease to 4,800 at Kampsville, 123 miles from Peoria. The river Rhone contains an average of 75 bacteria per c.c. above Lyons and 800 below. The Dee, 88 above Braemar and 2,829 per c.c. below. Many more similar results are found in the literature. LAKES. The water of lakes is generally much purer than river water. Near the shore, the bacterial content is higher than farther out, showing the contaminating influence of habitation. Thus Lake Geneva contains as many as 150,000 bacteria per c.c. near the shore, and further out only MICROORGANISMS IN WATER. 2OI 38 per c.c. Other figures are as follows: Loch Katrine, 74 per c.c., Lake Lucerne, 8 to 51 per c.c., Lake Champlain, 82 per c.c. SEA WATER. There are few bacteria in sea water remote from the coast; but near the shore and in the neighborhood of seaports there may be large numbers. Examples: 350 meters from Naples, sea water contained 26,000 bacteria per c.c. At a distance of 3 kilometers, only 10. Samples taken from depths of 75 to 800 meters at distances from 4 to 15 kilometers from shore were found to contain from 6 to 78 bacteria per c.c. in surface water, and from 3 to 260 at various depths below. CAUSES AFFECTING THE INCREASE AND DECREASE OF THE NUMBER OF BACTERIA IN WATER. There are a number of causes which influence the multiplication or diminution of microorganisms in natural waters; and while it is necessary to discuss each of these causes in detail, it must be remembered that a number of them may be simultaneously influencing the increase or decrease. TEMPERATURE. In natural waters, a low temperature probably acts injuriously on parasitic bacteria, reducing their numbers; but the bacterial content of water during the hot summer months is generally not so large as during the cooler seasons. Water collected for exami- nation should be analyzed at once; otherwise, contradictory results as to numbers will be found. Usually, in most waters, there is a reduction in numbers for a few hours, followed by a large increase. Very much polluted waters, however, show a marked decrease of intestinal organ- isms, if the samples are kept cool. LIGHT (page 162). Although the germicidal effect of sunlight is well known, yet it has not such powerful effects on the bacteria in water. Much depends, no doubt, on the turbidity and speed of the current, the maximum killing effect being produced in shallow, clear and slow- moving water. It has been found by experiment that the germ-killing power of light extends to a depth of three meters (about 9.84 feet). As a means of purifying water, direct light produces very little effect. FOOD SUPPLY. The amount of organic matter in water directly influences the growth of bacteria. Where a large amount of this is present, the number of microorganisms is also large. Rivers containing 202 MICROBIOLOGY OF WATER AND SEWAGE. considerable organic matter derived from vegetable debris, etc., contain, as a rule, more organisms than rivers in which there is but little of such material. Thus the Ottawa River, which drains a large area of forest lands and is characterized as an upland peaty water carrying a rather high percentage of organic and volatile matter, contains throughout the year a larger number of organisms to the cubic centimeter than the water of the river St. Lawrence, which is much clearer and contains much less organic matter. Sewage water is rich in organic matter, and proportion- ately rich in bacterial life; and bacterial purification is synchronous with a diminution of organic matter. Jordan remarks in this connection that "in the causes connected with the insufficiency or unsuitability of the food supply is to be found the main reason for the bacterial self-purification of streams." OXIDATION. On the surface of waters, in rapids, falls, and tidal rivers, much oxygen is absorbed, and much impure matter is thus oxidized. Such oxidation is one of the minor agencies in the purification of water. VEGETATION AND PROTOZOA. Low forms of plant and animal life, like certain species of algae, river plants, and the numerous protozoan forms, bring about a reduction of organic matter in water, and thus reduce the amount of food available for bacteria. There is also the antagonism between these forms and bacteria. The chemical products of the higher forms are considered by some authorities to be injurious to bacterial life; and many bacteria are ingested by predatory protozoa. DILUTION. Sewage flowing into a river or lake is at once diluted with quantities of pure water, and the amount of available food material is thus diminished; the space occupied by a definite number of bacteria is increased; and it is easy to see that the greater the dilution, the fewer sewage bacteria will be found. An example will suffice to illustrate. The sewage of the city of Ottawa amounts to about 454 1. (100 gal- lons) per second; and the gelatin count from it gives an average in round numbers of 3,000,000 bacteria per c.c. The yearly mean discharge of the river is about 1,364,511 1. (300,000 gallons) a second; and thus the sewage becomes diluted 3,000 times. SEDIMENTATION. Impurities, suspended matter, and bacteria having weight, naturally gravitate to the bottom; and the subsidence of these matters is spoken of as sedimentation. Lake water being still, sedimentation in it is more marked than in moving water; and such water contains but few bacteria. In slow- MICROORGANISMS IN WATER. 203 moving rivers the influence of this factor is also quite pronounced; and, according to Jordan, "The influences summed up by the term sedi- mentation are sufficiently powerful to obviate the necessity for summoning another cause to explain the diminution in numbers of bacteria" in sewage polluted rivers. The example already given (page 200) of the self- purification of the Chicago drainage canal illustrates Jordan's contention. OTHER CAUSES. There is a number of other causes, not well known nor of sufficient practical importance for more detailed comment, which may increase or decrease the number of bacteria in water, such as the inhibiting action of microorganisms and their products on one another, the effects of pressure, etc. A peculiar fact, which has never been satisfactorily explained, is the quick death (in three to five hours) of the cholera vibrio in the waters of the Ganges and Jumna. When one remembers that these rivers are grossly contaminated by sewage, by numerous corpses of natives (often dead of cholera), and by the bathing of thousands of natives, it seems remarkable that the belief of the Hindoos, the water of these rivers is pure and cannot be defiled, and they can safely drink it and bathe in it, should be confirmed by means of modern bacteriological research. It is also a curious fact that the bactericidal power of Jumna water is lost when it is boiled; and that the cholera vibrio propagates at once, if placed in water taken from wells in the vicinity of these rivers. INTERPRETATION or THE BACTERIOLOGICAL ANALYSIS OF WATER. In making any analysis of water, all data, such as the kind of water and the particulars regarding collection, transmission, sampling, rainfall, etc., should be given, as these are a great help in interpreting the results. One analysis is rarely sufficient; examinations should be regularly and systematically made. QUANTITATIVE STANDARDS. No absolute guide can be given to determine the potable quality of water from the number of microorganisms in it. It may, however, be safely assumed that high bacterial counts indicate a large amount of organic matter. The number of organisms growing in beef peptone gelatin at 20-22, and termed the "gelatin count," should be given. For deep wells and springs, this should not exceed 50 per c.c.; and for shallow wells and rivers, not over 500 per c.c. After rains or floods, these figures might be exceeded, and would not necessarily indicate dangerous pollution. 204 MICROBIOLOGY OF WATER AND SEWAGE. The number of organisms which develop on beef peptone aga incubated at blood heat, commonly termed the "agar" or "blood-heat" count, is perhaps more important than the gelatin count, as many water bacteria do not grow at blood heat, whereas sewage and soil organisms grow readily at this temperature. The agar count eliminates the water flora, but obscures the sanitary results by reason of the presence of soil bacteria. For deep waters, the agar count should generally not exceed 10 per c.c. ; and for surface waters, not over 100 per c.c. QUALITATIVE STANDARDS. The isolation and identification of specific disease organisms, such as typhoid and cholera microbes from water, is sufficient to condemn such a sample as unfit for use; but on account of many technical difficulties it is practically impossible to make such an examination. Apart from a few special cases, when it may be necessary to attempt the isolation of these pathogenic bacteria, the pres- ence of the colon bacillus (B. coli) in small amounts of water, is generally looked upon as significant and indicative of sewage pollution. The technical methods used in this isolation and numeration are many, and may be found in the works cited; but there is considerable difference of opinion as to the number of B, coli which should condemn a sample of water. Prescott and Winslow state that if the colon bacillus is in "such abundance as to be isolated in a large proportion of cases from i c.c. of water, it is reasonable proof of the presence of serious pollution." Savage suggests that B. coli should be absent from 100 c.c. in the case of water from deep wells and springs, and should be absent from 10 c.c. in surface waters, such as rivers used for drinking purposes, shallow wells, and upland surface waters. The streptococcus examination is next in importance as an indicator of sewage. Streptococci should be absent from the amounts of water mentioned above for B. coli; and B. enteritidis sporogenes should not be present in 1,000 c.c. of water from deep wells, nor in 100 c.c. from sur- face waters. SEDIMENTATION, FILTRATION, AND PURIFICATION OF WATER. As areas become more and more thickly settled and towns and cities increase in population, the problem of obtaining sanitary control over the water supply increases in importance. Very few towns and cities are fortunate enough to obtain their water supply from an unpolluted MICROORGANISMS IN WATER. 205 area. Consequently expensive installation must be made, in order to purify a suspiciously contaminated water by freeing it from organisms injurious to health. There are several methods of accomplishing such purification; and these will be briefly mentioned. SEDIMENTATION AND FILTRATION. This method of purifying water has been used for nearly a hundred years; but the great impetus given to this hygienic measure was due to Koch, who showed in 1893 that the FIG. 58. Section of a sand filter. proper filtration of Elbe water saved the town of Altona from an epidemic of cholera which devastated Hamburg as a result of drinking unfiltered water. In this system of purification, the water is first stored in large reservoirs, where the effect of sedimentation and storage reduces con- siderably the number of bacteria. From the reservoir, the water is filtered through sand, gravel, and pebbles, etc., arranged as shown in Fig. 58. This filtration removes from 97 to 99.5 per cent of the microorganisms. 2O6 MICROBIOLOGY OF WATER AND SEWAGE. Mean of Monthly Examinations for the Year. Microorganisms per c.c. At source After storage After filtration London Lambeth Works. . . 16 138 7 820 7C London, Chelsea Work. 16 138 i 067 / D 24. Berlin, Lake Miiggel I,4OO 60 Paris, Marne 7O,OOO 6^O Paris Seine .... 186 986 "0" AQQ The action of the filter bed is due to the mechanical obstruction of impurities, to oxidation of the organic matter, and to nitrification due to the living bacteria in the scum which forms on the top of the layer of sand. Of these, the last is the most important; for until this gelatinous layer forms, the filter does not act properly in fact, it has little filtering action, as the following figures show: 'Bacterial Content of Water Before and After Cleaning the Sand Filter. Before cleaning, i.e., before removing the scum layer .... 42 per c.c. One day after cleaning ". 1880 Two days after cleaning 752 Three days after cleaning 208 Four days after cleaning 156 Five days after cleaning 102 Six days after cleaning 84 Thus provision must be made to permit the scum or film to form before the filtered water is used for domestic purposes. The rate of filtration must be regulated; for if the water is allowed to exceed a certain rate (101.6 mm. or 4 inches per hour), inefficiency follows. COAGULATING BASINS AND FILTRATION. This method of purification consists in adding a coagulant, such as basic sulphate of aluminum, by means of a mechanical device which regulates the quantity, as the water is pumped into the coagulating basins or reservoirs, where it remains for six to twenty-four hours. The aluminium sulphate is decomposed by the lime in the water and forms insoluble aluminium hydrate; and the sul- phuric acid combines with the lime. The hydrate of aluminium is pre- MICROORGANISMS IN WATER. 207 cipitated in large flocculent masses, entangling all particles of soil or organic matter; and these, being deposited on the surface of the sand, form the filtering layer. Such filters are very efficient; they remove from 97 to 99.8 per cent of the bacteria from the water. POROUS FILTERS. (Fig. 59.) These filters are either made from unglazed porcelain or baked diatomaceous earth; the former are known as Chamberland, and the latter as Berkefeld filters. These filters are usually candle-shaped, require considerable pressure to force water FIG. 59. Unglazed porcelain niters. Chamberland system; A, without pressure; B, fitted to main water supply; C, section of a porous porcelain filter. through them, and can be used only when a small supply of water is needed. Water which is forced through these filters is at first sterile; but with repeated use they allow bacteria to pass through the pores and thus the filtering efficiency is impaired and will remain so, until the filters are cleaned and baked to red heat in a muffle-furnace. Unless this is done regularly, no dependence should be placed on these filters, as they only put those who use them off their guard against the danger to which they are exposed. PURIFICATION BY OZONE. The antiseptic properties of ozone are 208 MICROBIOLOGY OF WATER AND SEWAGE. well known. It is used in the purification of the water supply of some towns Nice, Chartres, etc. Ozone used for this purpose is usually obtained by means of the electric current; and a flowing film of water is brought into contact with an upward current of air charged with ozone, which current makes the water almost completely sterile. This method of purification is efficient, but rather expensive. PURIFICATION BY HEAT. By bringing water to the boiling point, all harmful bacteria are destroyed; a few spores may resist this treatment, but they are harmless. Boiled water is of a flat, insipid taste, due to the driving out of the contained gases. The taste may be improved by cooling and shaking. The boiling of water is often resorted to as a hygienic measure in times of epidemic, and for the supply of armies in the field. PURIFICATION BY CHEMICALS. The addition of a small amount of calcium hypochlorite, or potassium iodide, etc., purifies water; but these methods are seldom used, except for the use of soldiers on campaign. LOCATION AND CONSTRUCTION OF WELLS. Farms in many sections of this country are practically all supplied with surface water collected in shallow wells. Hence farmers should understand the principles involved in the location and construction of wells. Many farm wells are badly located too near such sources of contami- nation as out-houses, cess-pools, stables, or barn-yards; and those who locate them give too little attention to the slope of the ground, and the nature and slope of the subsoil. There should be at least 22 to 30 M. (75 to 100 feet) between the well and all probable sources of contamination; and this distance is too small, if the soil is very porous, or if the surface and subsoil drainage is toward the well, or if the well is sunk in fissured rock as it is obvious that there are serious chances of contamination in each of the above circumstances. In all cases, the surface drainage should be away from the well; and, as far as possible, the subsoil drainage also should be from the well. Sketches 60, 61, and 62 illustrate these points, the upper part of each drawing showing the plan and the lower portion a section through the dotted line marked on the plan. Figure 60, shows that the surface drainage is trom the house, privy, stables, and barnyard toward the well. The section fhrough the line "A" shows the relation of the impervious subsoil "B" to MICROORGANISMS IN WATER. 209 , 1 1 i 6 5 ^ _ / (_ FIG. 60. / ---A FIG. 61. FIG. 62. FIGS. 60, 6 1 and 62. In each figure plan above section through A B below. S = Soil; B=impervious subsoil or strata, i, .House; 2, well; 3, outhouse; 4, piggery; 5, stables; 6, stable yard; 7, hen house; 8, sheep stable. Arrow heads indicate direction of water flow. (Original.) 14 210 MICROBIOLOGY OF WATER AND SEWAGE. the drainage. Water falling on the surface of the ground would pene- trate through the soil to the upper portion of the subsoil, and then move along it in the direction of the greatest slope. In this sketch, the subsoil drainage is away from the well; and in this respect the well is located properly; but, in respect to the surface drainage, improperly located. A better place for the well would be at the letter "X." In Fig. 61 the surface drainage including that from the adja- cent outhouse at 3, which is too close to the well is toward the barn, and away from the well; but the subsoil drainage from all the buildings, Soil FIG. 63. Construction of a model well. On the right is brick construction, on the left stone construction, as illustrated. (Original.) except the house, is in the direction of the well; and thus contamination of the water supply is liable to occur. Fig. 62 shows a well properly located as regards both surface and subsoil drainage. Such a well will supply pure water, if it is properly constructed. Figure 63 shows the proper construction of a well with brick or stone. Large vitrified drain pipes with cemented joints will answer equally well when there is an abundant supply of water; but in case the supply of water is limited, a large area is needed, and a stone or brick well is necessary. MICROBIOLOGY OF WATER. 211 Reference to the illustrations will show that every endeavor is made to prevent surface water from entering directly into the well. The walls are impervious; and the earth or clay is well rammed against the outer side of the wall. The curb is carried well above the surface of the ground. The waste water is conducted by means of a sloping platform, trap, and drain, away from the well; and the well opening is properly covered. All water entering such a well must percolate through a considerable depth of soil, and undergo purification by means of the aggregations of living bacteria in the soil spaces. Thus the soil around a well fulfils the same function in purifying the surface water as the scum layer that forms on the surface of gravel filters. CHAPTER II.* MICROBIOLOGY OF SEWAGE. THE BACTERIAL FLORA OF SEWAGE. COMPLEXITY OF FLORA. Sewage is made up of the miscellaneous and varied wastes of human life and activity, and the bacteria which are found therein are the result of a haphazard and chance admixture of sub- stances of diverse origin and character. The resulting flora is not only of great diversity and variability, but it is with few exceptions non- characteristic. In brief, the medium with which we have to deal has had an origin too indefinite and a history too short to have permitted the establishment of anything approaching a constant or characteristic bacterial flora. TYPICAL FORMS. Our interest in this sewage flora is a very practical one, being confined to those organisms which carry on the work of biological purification and to certain pathogens which for obvious reasons require special treatment. We are interested chiefly in what these bacteria do rather than in what they are, and our classification is influenced accordingly. It is based, not upon the species or the genus nor even upon the group or type, that proves so convenient in general bacterial classification, but upon a sort of physiological or functional type, having to do solely with the activities of the organisms in sewage and in its purification. Bacteria performing a common function or producing a common result are members of one type. Individuals may belong to several of our types and there are doubtless a great many that belong to none. These latter simply have no place assigned them as yet in the role of sewage purification, because they possess none of the recognized typical functions. Apparent exception may be taken to these general principles in the case of such organisms as the B. coli, sewage streptococci and B. enter itidis. These are, to a certain extent, characteristic sewage bacteria. But interest in them as individuals is confined to water bacteriology. If they have any functions in the bacterial changes of sewage, they receive attention as members of a corresponding type, not * Prepared by Earle B. Phelps. 212 MICROBIOLOGY OF SEWAGE. 213 as individuals. A study of these sewage types, therefore, is a study of the chemical changes induced in the medium by the activities of one or the other group of bacteria. TYPES OF SEWAGE BACTERIA. According to the general character of the changes which they bring about, sewage bacteria are divided into two large groups, the anaerobic or putrefactive bacteria, and the oxidizing bacteria. In regard to the former, no attention is paid to the fine distinctions that have been made in recent years in connection with the definition of putrefaction. In sewage chemistry putrefaction is that change which takes pi ace naturally in sewage after anaerobic conditions have become established. It in- volves the reduction of urea, the hydrolysis of protein and of cellulose, the emulsification of fats, the reduction of nitrates and sulphates and possibly of phosphates, and those other changes which are characterized by the withdrawal of oxygen and the hydrolysis of complex molecules. These changes are always noted in sewage under anaerobic conditions and the terms putrefactive and anaerobic change are for the present purposes practically synonymous. The oxidizing reactions on the other hand might be classed under the general heading of aerobic reactions, except that they constitute only a small portion of the group of reactions which take place normally under aerobic conditions. They are distinguished by the fact that oxygen is added to the molecule, the product always containing more oxygen than the initial substance. Carbon dioxide, water and nitrates are produced, in distinction from methane, hydrogen and ammonia, which characterize the anaerobic reactions. A third type, possessing objective rather than subjective functions, in sewage, is made up of pathogenic and other harmful bacteria. These play no part in our theories of purification and the proof of their presence is generally lacking. For the protection of the public health, it is assumed that they are always present in sewage, and our procedure in sewage disposal is modified throughout in accordance with this assumption. With these definitions in mind we may proceed to a more detailed study of the bacterial types themselves. PUTREFACTIVE AND ANAEROBIC BACTERIA. Putrefaction or anaerobic fermentation involves the withdrawal of oxygen from one molecule or part of a molecule and the subsequent oxidation of another molecule or 214 MICROBIOLOGY OF WATER AND SEWAGE. part of the same molecule. The energy released in this process is utilized in the vital functions of the organism. This action is neither oxidation nor reduction, or more strictly, it is both taking place simultaneously. A good example of such a process is the fermentation of urea. The reaction takes place as follows: CO(NH 2 ) 2 + 2 H 2 O=(NH 4 ) 2 CO 3 . Carbon is oxidized at the expense of hydrogen, a process which, by itself, is endothermic, that is, requires heat or energy for its maintenance. But the heat of formation of the final product is greater than that of the initial substances and the energy thus liberated becomes available for use by the bacteria. It is in this way that hydrolytic changes of this character play the same role in anaerobic reactions that is played by direct oxida- tion under aerobic conditions. The Liquefaction of Protein. One of the most clearly defined and useful types of bacterial activity to be seen in the various sewage disposal processes is that which we term liquefaction. This term is used to denote broadly all those changes by which solid and insoluble organic matter is converted into a soluble condition. The particular process known as protein liquefaction is in the main analogous to gastric digestion. Its one characteristic is the increased solubility of the product. The practical importance of protein liquefaction in sewage disposal is very great and the value of the liquefying bacteria correspondingly high. Nevertheless, % aside from our knowledge of analogous processes in digestion and in bacterial putrefaction of albuminous substances, we know almost nothing of the chemistry or the bacteriology of this process. An enormous variety of bacteria are included in this group. The whole process is doubtless the result of a very complicated symbiosis in which various sub- groups of bacteria carry out the initial reaction, from which point other groups carry it through successive stages. Absence of one or another of these groups or of some important species of any group doubtless accounts for the diverse results that are recorded. It is well known that the activi- ties within a septic tank, for example, are seldom twice the same. Gross differences readily apparent to the senses of one versed in such matters certainly exist, and in actual results it is rare to find two tanks doing exactly the same kind of work. Much depends of course upon the chem. ical character of the sewage itself, but much, that is still unexplained, must eventually be traced to the great diversity of the sewage flora and the com. MICROBIOLOGY OF SEWAGE. 215 plex symbioses as well as bacterial antagonisms that are involved in the reactions with which we are dealing. During these reactions proteins and albumins are hydrolyzed by suc- cessive stages to albumoses, peptones, amino-acids, amines, and finally to ammonia, carbon dioxide, methane, hydrogen, etc. Simultaneously am- monia, amines, and carbon dioxide are eliminated at each stage as side products. The tendency then is toward simple, soluble and gaseous products, and hence of value in the preliminary resolution of the sewage. The Fermentation of Cellulose. The fermentation of cellulose is, next to protein hydrolysis, the most important work of the anaerobic bacteria in sewage treatment. So far as is definitely known this action is usually confined to anaerobic conditions. The fact that fence posts decay first at the surface of the ground, or that wood in general decays more rapidly when it is exposed to only a slight degree of moisture, than when it is immersed in water is only an apparent contradiction. The conditions are aerobic in both cases and aerobic bacteria would not be favored by total immersion but the effect in both instances seems to be due to fun- gus growths which are more active in the moist wood. The anaerobic fermentation of cellulose is that which is found typically in marshes and of which the chief products are carbon dioxide and methane or "marsh gas." Nitrogenous food material is also requisite, which accounts for the preserving property of reasonably pure water upon wood. In the septic tank the solution of cellulose is extremely rapid, and large pieces of cotton cloth or rolls of paper are completely dissolved within a few months. Wood itself is more resistant and withstands the action of the tank for years. This is largely due to the fact that the wood molecule is much more complicated than a simple cellulose molecule, and, among the conifers at least, to the further fact that antiseptic intercellular substances are present. Chemically considered the action is hydrolytic and can be imitated by prolonged boiling in dilute acids. Pectin substances, starches and finally sugars are produced while butyric and other organic acids, carbon dioxide and methane appear as by-products. Bacteriologically, although it has variously been ascribed to one or another organism, it is probably the result of the activities of many and is possibly not the principal activity of any one of these. In other words, cellulose fermentation is probably a 2l6 MICROBIOLOGY OF WATER AND SEWAGE. series of side reactions produced during the fermentation of the ni- trogenous material rather than a definite reaction upon which the met- abolism of any single species depends. This view is strengthened by the general observations that this fermentation is in most cases due directly to enzymes. Viewed in this light it is easy to understand the difficulty that has surrounded the isolation of definite cellulose fermenting organ- isms. Many have been described, chief of which are B. butyricus or B. amylobacter, B. omelianski, Sp. rugula. The Saponification of Fats. A third great group of type reactions occurring under anaerobic conditions is the saponification or splitting of fat. Our knowledge of this process is even less definite than of the cellulose fermentations. It is a fact that there does take place in sewage a gradual saponification and emulsification by which the fat loses its identity and mingles with the liquid. This effect is most noticeable in the case of long sewers in which considerable velocities are maintained. In quiescent tanks there is a tendency for the fats to rise to the surface and thus become removed from the influence of this action. Thus in small installations enormously heavy scums form upon the tanks and analysis shows a considerable percentage of fat in this material. In larger systems on the other hand there is less and less evidence of fatty material as such. It is true that there is a deposit upon the walls and tops of such sewers and that small floating objects, like matches, rolling along such a wall will accumulate layers of grease and become eventually the familiar "grease- balls" found in the discharge, but in the main the fatty material has be- come well disintegrated before the outlet is reached. In this case also as in that previously discussed it is not believed that the action is a direct result of the activity of any particular organism. The proteolytic changes are accompanied by the freeing of alkaline products, ammonia and amines, which leads to some saponification, and which, in turn, leads to a further emulsification. Whether specific enzymes are present which assist in this final process or not has never been determined. It is significant to note, however, that where sewages are slightly acid, unaltered fats are much more abundant, even though the acidity is insufficient to prevent vigorous putrefactive changes in the sewage itself. The Fermentation of Urea. The fermentation of urea has already been referred to as a typical and simple case of anaerobic decomposition. This reaction has great significance in sewage chemistry since a consider- MICROBIOLOGY OF SEWAGE. 21 7 able proportion of the nitrogen of sewage is present initially as urea. Owing to the ease and rapidity with which the reaction takes place, however, no special effort is necessary to bring it about in sewage treatment and it therefore receives brief attention in discussions of the chemistry of sewage. The change to ammonia takes place in the small sewers of the system and it is difficult and generally impossible to detect the presence of urea in sewage. It has even been suggested that certain enzymes present in fecal matter are instrumental in bringing about this change and that the bacteria are only indirectly concerned. It is known, however, that a large number of bacteria of general occurrence have the power to produce this fermentation. Of these the Bad. uretz (Miquel) may be cited as an example. The Reduction of Sulphates and Nitrates. The production of sulphuretted hydrogen during the anaerobic decomposition of sewage is commonly noted. This substance may arise in at least two ways. Sulphur, being a constituent of most protein substances, is split off from the molecule in this form during certain types of fermen- tation. Its formation in these cases is analogous to that of ammonia from protein. The amount so produced is small and is usually neutralized and precipitated by the small amounts of iron and other metals always present in sewage. There is therefore no liberation of the gas itself and it is often said that sulphuretted hydrogen is not formed normally in a septic tank. This conclusion is readily disproved by a simple test of the black residue found at the bottom of such tanks. A second and more important source of this substance is the sulphate normally present in many sewages. Throughout many parts of the country the water supply contains material quantities of magnesium or calcium sulphate, and upon the sea coast the sewage generally receives more or less salt water. In these cases the reduction of sulphates to sulphuretted hydrogen is not only of interest bacteriologically but probably exerts an influence upon all the reactions that are going on simultaneously. In fact this example serves excellently to illustrate the great complexity of these anaerobic reactions and the mutual interdependence of each upon all the others. Sulphates, under anaerobic conditions, are a source of oxygen and it is upon oxygen that the course of all these reactions depends. Therefore the presence of sulphates and the possibility of their yielding oxygen may 2l8 MICROBIOLOGY OF WATER AND SEWAGE. alter the course of the other reactions involved. The products of the protein hydrolysis for example may be profoundly modified by the pres- ence of this additional source of oxygen. The effect upon the bacteria themselves is also to be considered as a factor quite distinct from the purely chemical effect just described. It has frequently been observed, and in fact would be expected, that the products of anaerobic putrefaction are themselves detrimental to the activ- ity of the organism producing the changes in question. The nature of sulphuretted hydrogen makes it appear quite probable that we are dealing here with a toxic substance that would at least inhibit the activities of certain bacteria and in this way further modify the final result. The same might be said of almost all the reactions with which we have to deal but this example is cited as a typical one. It is known in practice that the presence of sulphates in a sewage does lead to a distinct type of anaerobic change which is characterized by the marked blackening of the sewage, the formation of secondary reaction products which precipitate after the removal of the suspended matter of the sewage, the evolution of hydrogen sulphide, an excessive amount of mineral or non-volatile residue in the sludge and the formation of free sulphur upon subsequent aeration of the sewage. Here again, as in the other types of reaction, it is useless for the present to attempt to ascribe this reaction to any particular species. Sp. desulphuricans and B. sulpliurens have been isolated. A non-liquefying anaerobic bacillus, which reduced sulphates strongly, was isolated from Boston sewage in the writer's laboratory by G. R. Spaulding. -Others have been described and there is undoubtedly a large group of organisms capable of bringing about the reaction. Just as the reduction of nitrates is a function performed by many, perhaps most, anaerobes, so the reduction of sulphates, although a less common function, is still common to many forms. In fact nitrates, sulphates, and phosphates form a series in regard to their reducibility and the effect of their presence upon the reaction as a whole. The phos- phates so far as has been recorded are not ordinarily reduced. OXIDIZING BACTERIA. The Production of Nitrate and Nitrite. A long series of investigations upon the organisms which oxidize nitrogen began with the Franklands and Winogradski, and has continued to the present day. These have given us much information concerning the MICROBIOLOGY OF SEWAGE. 2IQ habits and functions of the nitrifying organisms. Winogradski 's original types were Nitrosomonas and Nitrobacter, the former oxidizing ammonia to nitrite, the latter completing the oxidation to nitrate. Work upon these organisms constitutes such an important factor in soil bacteriology to-day that more detailed discussion of this nitrifying function is left for another place. In the earlier days of sewage purification great stress was laid upon the work of these organisms, which was believed to be fundamental. The degree of nitrification was accepted as a measure of the work of the filters and little thought was given to the possibility of oxidizing reactions by other forms. With the development of modern sewage disposal methods, the work of this latter type of bacteria has assumed a more important role and the actual work of the nitrifying organism has been found to be of only minor and incidental importance. Other Oxidizing Reactions. The great groups of aerobic and facultative bacteria are in general concerned in the oxidation of organic matter. There is nothing specific in this reaction and very little that is character- istic of any special or smaller groups. Under certain special and restricted conditions, typical products are formed by particular species, as in the manufacture of vinegar, and it is possible that a careful study of the com- plex reactions involved in the oxidation of sewage would show a certain sequence in the order of events and certain definite work being accom- plished by definite groups. In other words, symbiosis and specializa- tion doubtless take place to a limited extent. But the fundamental fact remains that the metabolism of the organism demands that organic matter be oxidized for the production of energy. Even though certain food substances may be preferred and certain decompositions be norm- ally produced there is necessarily a great latitude and great adaptability. For this very reason a study of the individual organism and its action upon specific materials throws no light upon the major problem, which is, given fifty different types of organisms and fifty different fermentable substances, in a mixture, what will be the course of the reaction. Here the preferences, the adaptability and the antagonisms all come into play and while it is impossible to say what has happened or how, it is readily conceived and, in fact, almost apparent, that out of this heterogeneous mixture there will come a homogeneous symbiotic family and an orderly sequence of chemical events, in which metabolic needs and food supply are all delicately adjusted. 220 MICROBIOLOGY OF WATER AND SEWAGE. PATHOGENIC BACTERIA. Prevalence and Longevity. Owing to its origin and nature, sewage may at any time contain infectious material and for the purposes of the sanitarian it is assumed that at all times the germs of disease are present. Such an assumption is possibly in excess of the actual facts and is only justified because it supplies the only possible hypothesis having an adequate margin of safety. The actual prevalence of pathogenic bacteria obviously depends in the first instance upon the amount of sickness in the contributing community. Furthermore, if, as we are coming to believe, a definite proportion of the population are perpetual carriers of typhoid infection then to just as definite an extent is the bacterial population of the sewage made up of typhoid bacteria from apparently well persons. In addition to these, about five one- hundredths of i per cent of the population of American cities are suffer- ing from the disease in acute form. Making due allowance for the extra precautions that are, or should be taken in the care of the dejecta, these persons constitute a definite and fairly constant source of infection. In the case of the other infectious diseases of the alimentary tract, and, possibly to a less extent in the case of tuberculosis, diphtheria, and many others, these general statements are equally applicable, so that the possibility of the occurrence of infectious material in sewage is not a remote one, but definite and almost quantitatively determinable. As to the persistence of active pathogenic bacteria in the sewage for any length of time the data are less exact. In the case of typhoid fever, which has been more carefully studied than any other disease, the germs are more persistent in pure water than in impure, but whether this general- ity can be extended to sewage is debatable. Our best information leads to the belief that any reduction in numbers of typhoid bacteria which may take place within the sewer before discharge is of minor importance and of slight sanitary significance. Discussion of other pathogens must be in even more general terms. Information is almost wholly lacking and it can only be assumed for purposes of safety that, in so far as organisms of these various types are discharged into the sewer, they will persist to a certain extent in the sewage until it is finally disposed of. If such disposal be by discharge into a stream without purification, then the waters of that stream become pol- luted with infectious material. Studies recently made by Sedgwick and McNutt have indicated the possibility that many diseases, other than the oft-quoted typhoid fever, may be transmitted in this way. MICROBIOLOGY OF SEWAGE. 221 Life in Septic Tanks and Filters. With the introduction of the septic tank at Exeter, England, in 1893, the question of the fate of pathogenic bacteria in such a tank was raised. It was even suggested that bacteria, such as the typhoid organism, might multiply in the tank. The question was investigated by Professor Sims Woodhead, who concluded that no organisms capable of setting up morbid changes in animals were dis- charged from the tank. This negative evidence however has little weight in the light of more recent experiments. Pickard introduced an emulsion of typhoid bacteria into this same tank and noted only a gradual decrease. After fourteen days he was able to detect i per cent of the initial number. He also reported a removal of 90 per cent of the typhoid organisms in- troduced into a contact filter. These data must be interpreted in the light of two established facts. The typhoid organism tends to die at a rapid but diminishing rate under any but the most favorable conditions. This results in a rapid decrease at first, with a prolonged survival of a few individuals. This process takes place in sewers, in streams, and, in fact, under most artificial conditions. The second fact of importance is the difficulty of recovering the typhoid organism under experimental conditions like those described. A thorough study of the bacteriology of sewage and of filter effluents led Houston to conclude that the biological processes at work in a filter or tank were not strongly inimical, if hostile at all, to the vitality of path- ogenic germs. A conservative study of all the evidence bearing upon this important question including the vitality and fate of certain non-pathogenic species, such as B. coli, leads to the conclusion that the removal of pathogenic bacteria in purification methods is due to two allied causes, the efficiency of which can be approximately determined. There is first the time element and the known rapid decrease in the numbers of certain bacteria such as B. typhosus when placed under conditions that preclude multipli- cation. The rate of decrease varies but is roughly about 50 per cent in twenty-four hours. The second factor, acting in reality in conjunction with the first, is the mechanical hindrance that is offered to the free passage of suspended materials through the body of a filter. Even fine sand offers little strain- ing action as such, since the open channels are thousands of times as big as the bacterial cell, but surface tension phenomena tend to make all solid material adhere to the medium and thus its passage is delayed. 222 MICROBIOLOGY OF WATER AND SEWAGE. This action is prominent although of less importance in coarse-grained filters. Actual experiments by the writer have indicated that while the liquid may pass through a trickling filter in half an hour, small suspended particles such as ultramarine and B. prodigiosus cells require an average of over twenty-four hours. In this way the actual time of passage is greatly delayed even when coarse broken stone is the filter medium, and the times that are now known to be necessary for the passage are ample in themselves to account for the reductions that have been noted. It may therefore be stated as a conservative view of the efficiency of purification processes in the removal of pathogenic bacteria, that there are no strongly inimical processes at work in the tanks or filters, and that the rate of decrease is not materially greater than would be observed in the same period of time under the conditions of a running stream. THE CULTIVATION OF SEWAGE BACTERIA. There are two general methods employed for the cultivation of those bacteria which are of assistance in sewage purification. They may be cultivated in so-called filters of sand or coarser material, or in specially constructed tanks such as the septic or the hydrolytic tank. In the for- mer case the bacterial growth occurs upon the special medium provided, the sand or stone; in the latter, it takes place in the liquid itself and a continuous life history within such a tank is possible only when the rate of flow is sufficiently slow to permit of the inoculation of the incoming stream by the contents of the tank. FILTERS. The filtering media most commonly employed are sand or crushed stone or other coarse material. In natural sand beds a brief period of treatment with sewage suffices to produce an active state of "nitrification." By this term is indicated all the complex processes of oxidation one index of which is the formation of nitrates. After such a filter has once become active in this way it will continue, with proper care, to oxidize sewage almost indefinitely. Improper care, such as an over- dose of sewage or continued flooding of the surface due to poor drainage, will soon destroy the activity of the filter. The addition of germicidal substances has a similar effect and cold weather somewhat reduces the efficiency. From all this it is apparent that a filter is a biological culture medium upon which the various types of bacteria are growing and carry- ing out their functions and that such a medium requires careful control and is sensitive to unfavorable changes in environment (Fig. 64). MICROBIOLOGY OF SEWAGE. 223 The other filters are similar to this and illustrate the true function of filtration. In the case of the sand filter it might be maintained that filtration or straining was an essential element in the process, but in the case of these coarse-grained media straining action is eliminated. Here there is nothing but a pile of stones, varying from one to three inches or more in diameter, upon the surface of which the bacteria grow. The FIG. 64. Sewage Experiment Station, Mass. Inst. Technology. Trickling filter in front, sand filter just behind trickling filter, dosing tank just behind sand filter, and septic tank just behind dosing tank. sewage trickles slowly over the surfaces, or is held in contact with them temporarily, according as we are dealing with trickling or contact filters. Solids adhere to the stones or settle upon them, and soluble material is "absorbed" by the surface growth and removed from solution. Within these gelatinous growths to which the air also has free access, the pro- cesses of oxidation take place and the products, the semi-oxidized organic 224 MICROBIOLOGY OF WATER AND SEWAGE. material, are later "shed" from the stones appearing again in the effluent as humus or stable organic matter. ANAEROBIC TANKS. The cultivation of bacteria in anaerobic tanks is not quite as simple a matter as that which has just been described. The sewage is allowed to flow slowly through the tank and after some time, from a few days to a month or more, a normal and constant flora will have become resident there. This flora will soon have become so well established that the incoming sewage laden with a flora of its own mingles with a liquid in which the established flora is so greatly in excess that the Siphon Chamber- Chamber FIG. 65. Sketch of septic tank. (Original.) former in large measure gives way to the latter. In this way, while the sewage itself moves onward and is gone within a few hours, the flora is constant and persistent. A further aid in preserving this constant flora is the sludge at the bottom, in which the bacteria lodge and multiply and from which they are carried upward by the ever moving eddies and con- stantly re-inoculate the liquid above (Fig. 65). THE DESTRUCTION OF SEWAGE BACTERIA. BY BIOLOGICAL PROCESSES. Reference has already been made to the effect of biological processes of purification upon pathogenic bacteria. What was stated in regard to the pathogens is equally true of the sewage MICROBIOLOGY OF SEWAGE. 225 bacteria as a whole. Their destruction is due to time and an environment unfavorable to growth, rather than to any specific cause. Further evi- dence of these facts may now be given. Bacteria as a whole do pass even the fine-grained filters in large numbers. Careful analyses of their types show them to be a haphazard mixture from the original sewage flora with little or no observable selection. Houston pointed out the relative abundance of the streptococci, supposedly delicate organisms, and found on the whole that the relative abundance of the different kinds of bacteria seemed to be much the same in the effluent as in the crude sewage. On the whole we may conclude that the biological processes remove bacteria not by any specific antagonistic action but by delaying their passage and permitting the natural decrease that occurs when multiplica- tion is prevented. The more efficient the mechanism of the filter in producing this delay the more complete will be the removal. BY CHEMICAL PROCESSES. A much more reliable and economical * method for bacterial destruction is now available in chemical disinfection of sewage effluents. The writer's studies at Boston, Baltimore and elsewhere have shown that the application of hypochlorite of calcium in amounts depending upon the character of the effluent, and ranging from one to five parts per million of available chlorine (25 to 125 pounds of bleaching powder per million gallons), will produce a bacterial removal amounting to 98 or 99 per cent. This disinfectant is the most efficient of the known germicides, cost being considered. By this means it is possi- ble to practically eliminate the bacteria, good and bad, from an effluent and it is no longer necessary nor desirable to seek high bacterial removals in the purification process proper. By thus dividing the work of purifica- tion into its component parts each part can be carried out at a maximum of efficiency and economy. DIVISION HI.* MICROBIOLOGY OF SOIL. CHAPTER I. * MICROORGANISMS AS A FACTOR IN SOIL FERTILITY. INTRODUCTION. Rational views on soil fertility were first presented, in a systematic way, by Justus von Liebig in 1840. In his " Organic Chemistry in its Applica- tions to Agriculture and Physiology" he developed important theories on the circulation of carbon and nitrogen in nature, and on the function of the so-called mineral constituents of plants. When Liebig 's book appeared many of the leaders and students of agriculture still believed that humus, the partly decomposed residues of plants and animals in the soil, was the direct food of crops. They believed that soils could yield poor or rich harvests in proportion to the amount of humus present in them; they believed, in other words, that plants, like animals, used organic substances as food. Liebig rendered a great service to agriculture in emphasizing the sig- nificance of decay processes. He made it evident that humus as such is of no use to plants, and that it becomes valuable only in so far as it is resolved into the simple compounds carbon dioxide, ammonia, nitric acid and various mineral salts. To be sure, he regarded the decomposition of organic matter as a phenomenon purely chemical, nevertheless he succeeded in showing that decay, putrefaction and fermentation are funda- mental facts, connecting links between the world of the living and the world of the dead. The research of the following decades brought to light the intimate relation existing between microorganisms and the decomposition of * Prepared by Jacob G. Lipman with exception of sub-chapter on " Soil Inoculation" which has been prepared by S. F. Edwards. 226 MICROORGANISMS AS A FACTOR IN SOIL FERTILITY. 227 organic matter. In the realm of soil fertility the new discoveries revealed the vastness of the task assigned to soil microorganisms in providing available food for crops. It was shown that under the attack of bacteria and of other microorganisms the various organic debris in the soil are split into relatively small chemical fragments; that the carbon is restored to the air as carbon dioxide; that the nitrogen is changed into ammonia, nitrites and nitrates. It was shown, further, that in this breaking down of organic matter the various cleavage products, and, particularly, carbon dioxide, hasten, to an amazing extent, the weathering of the rock particles and make available thereby the mineral portion of plant food. It was shown, likewise, that apart from accomplishing the transformation of unavailable into available plant food, microorganisms are concerned also in the addition of nitrogen compounds to the soil. The evidence gathered slowly by many investigators made it plain, therefore, that microbes are an important factor in the growing of cultivated and uncul- tivated plants. Hence, the important place assigned to microorganisms in the study of soil fertility problems. THE SOIL AS A CULTURE MEDIUM. Arable soils present so wide a range of conditions as to modify, materially, the development and predominance of different species. Variations as to moisture, temperature, aeration, reaction, food supply and biological relations are important, in each case, in determining the survival or disappearance of any particular species. For this reason, the study of soil microorganisms must reckon with the mechanical composition of soils, their ability to retain water and their content of inert and soluble plant food. MOISTURE RELATIONS IN THE SOIL. AMOUNT AND DISTRIBUTION OF RAINFALL. Precipitation in different regions of the earth's surface varies from practically nothing to more than 1,524 cm. (600 in.) per annum. A portion of this water runs off the surface into the nearest stream, another portion is rapidly changed into vapor and is returned to the atmosphere, and the remainder passes downward, into the soil and becomes the medium in which plant food is dissolved. It is estimated that only about half the total rainfall percolates through the soil. Where the soils are open and nearly level 228 MICROBIOLOGY OF SOIL. the proportion of percolating water is relatively greater; where the soils are fine-grained and more or less impervious, or the topography broken, the proportion is relatively smaller. Bacteria and other microorganisms, as well as the higher plants, are directly influenced by the amount of moisture available for their various needs. Hence soil microbial activities are affected not alone by the amount of rainfall, but also by its distribution. It is obvious, for instance, that an annual rainfall of 762 mm. (30 in.) distributed rather uniformly throughout the year would produce different soil-moisture relations than the same amount of precipitation confined to only two or three months. As is pointed out by Abbe, a daily precipitation of 2 mm. (.079 in.) distributed throughout the three summer months would be quickly changed into vapor, and would hardly wet the soil; whereas the total quantity of 180 mm. (7 in.) evenly divided into ten or twelve rains would penetrate the soil to a considerable depth, and would furnish very favorable conditions for microbial development. In a similar manner it is pointed out by Hilgard that Central Montana, and the region in the vicinity of the bay of San Francisco, have each a total precipitation of 610 mm. (24 in.). But while in Montana the rainfall is distributed over the entire year and irrigation becomes necessary, the precipitation near San Francisco is limited to the portion of the year that nearly coincides with the growing season, and crops are enabled to mature without irrigation. RANGE OF SOIL MOISTURE. Any given volume of dry soil consists of solid particles separated by empty spaces. The sum of these spaces is known as the "pore-space." It varies from about one-third of the entire volume in coarse sands to more than two-thirds in pipe clay. In peat and muck it may amount to as much as 80 or 90 per cent, of the entire volume. Under air-dry conditions each soil grain is surrounded by a very thin film of moisture designated as hygroscopic water. When air-dry soil is moistened the films around the soil particles become thicker and finally cease to be isolated. A continuous liquid membrane, as it were, is stretched from particle to particle, and the surface tension that thus comes into play is capable of lifting large amounts of water to the surface. The continuous film of soil water that can hold its own against the pull of gravity is known as capillary water. Finally, when the liquid films around the soil grains increase in thickness beyond a certain point, the attraction between the molecules in the soil grains and the more MICROORGANISMS AS A FACTOR IN SOIL FERTILITY. 229 distant molecules of water is no longer great enough to overcome the force of gravitation, and the excess of water percolates downward. The water more or less readily moved by gravitation is called hydrostatic water. For any given conditions of the soils the amount of hydrostatic, capillary and hygroscopic water is directly dependent on their mechanical structure. It is evident that the aggregate surface of the particles in a fine-grained soil is much greater than that in a coarse-grained soil. Actual determinations have shown that the aggregate inner surface of one cubic foot of coarse sand may be but a fraction of an acre; whereas the same quantity of the finest clay may have an inner surface equivalent to three or four acres. These differences are to be expected, since, as is shown by Lyon and Pippin, i g. of fine gravel may contain 252 particles; i g. of medium sand, 13,500 particles; i g. of very fine sand, 1,687,000 particles; i g. of silt, 65,100,000 particles, and i g. of clay, 45,500,000,000 particles. Since the soil water is spread as a film over the solid particles and varies in amount with the fineness or coarseness of the soil, and since the quantity of plant food going into solution is determined largely by the amount of water in contact with the soil particles, it follows that clay soils will, under the same conditions, contain more plant food in solution than loam soils and still more than sandy soils. From the standpoint of soil microbiology this is important, for the microorganisms live and multiply in the film water surrounding the soil particles. The concen- tration of salts in this film water as well as their composition must of necessity affect bacterial activities. In the same way, methods of tillage and cropping affecting the concentration and composition of the film water will modify the chemical changes caused by bacteria. EFFECT OF DROUGHT AND OF EXCESSIVE MOISTURE. Optimum conditions for plant growth and the development of many important soil bacteria are furnished when about half of the entire pore space is filled with water. In light sandy soils the optimum moisture content may be reached when the wet material contains scarcely more than 8 to 10 per cent of water by weight; while in silt and clay soils the optimum may reach 16 to 20 per cent or even more. Continued depletion of soil moisture by plant roots and evaporation at the surface causes the film of capillary water to stretch more and more. Finally it becomes very thin, breaks, and ceases to be continuous. The 230 MICROBIOLOGY OF SOIL. soil then becomes air-dry and contains only hygroscopic water. It is estimated by Lyon and Fippin that, under average conditions of humidity, light sand will contain 0.5 to i per cent of hygroscopic moisture; silt loam, 2 to 4 per cent; and clay, 8 to 12 per cent. The amount of water present in air-dry muck or peat may range up to 40 per cent, or even more. According to Hall the film of hygroscopic moisture is about o.75/( (0.00003 in.) thick. As the soil dries out bacterial activity is sus- pended and many vegetative cells undoubtedly perish. Nevertheless, it will be seen that the moisture film even in air-dry material is deep enough to allow the bacteria a reasonable degree of protection. This will account for the survival of non-spore-bearing bacteria in dry soil for a long time. Indeed, instances are on record of the isolation of Azotobacter and Nitro- somonas from soils that had been kept in a dry state in the laboratory for several years. It may be noted, in this connection, that in the pro- cess of drying the soluble salts in the soil may be sufficiently concentrated in the thin films to cause plasmolysis and the destruction of individual cells. On the other hand, excessive moisture in the soil is not only directly unfavorable to aerobic species in that it limits their supply of oxygen, but is objectionable because it encourages the formation of reduction products that are toxic to these species. It is apparent, therefore, that favorable conditions for the formation of available plant food by bacteria are created when a certain relation is established between the volumes of moisture and air in the soil. The shifting of this relation in one direction or another is bound to react on species relationships and numbers. AERATION. MECHANICAL COMPOSITION or SOILS. Soil ventilation is an impor- tant factor in crop production. It provides for the proper supply of elementary oxygen so essential to decomposition processes in normal soils; for the supply of elementary nitrogen required by nitrogen-fixing species; for the removal of excessive amounts of carbon dioxide; and for the destruction of various toxic substances. The intimate relation existing between soil ventilation and the mechanical composition of the soil material is bound to react on the microbial factors involved. It is well known that the rate of flow of air through soils is inversely propor- tional to the fineness of the material; in other words, the fine-grained MICROORGANISMS AS A FACTOR IN SOIL FERTILITY. 231 soils, notwithstanding their greater pore space, will not allow air to pass through them as rapidly as coarse-grained soils. King shows, for in- stance, that 5000 c.c. of air passed through a column of fine gravel in thirty-seven seconds, whereas in similar columns of medium sand, fine sand, loam and fine clay soil the same amount of air required for its passage 1,178, 44,310, 282,200, and 2,057,000 seconds respectively. AEROBIC AND ANAEROBIC ACTIVITIES. The more rapid diffusion of gases from open soils naturally leads to a more frequent renewal of their oxygen supply. In its turn, the latter affects the ratio of aerobes to an- aerobes; it follows, therefore, that in clay soils and clay loam soils the activities of aerobic species are retarded to a greater extent than they are in sandy loams or sandy soils. It follows, also, that in fine grained soils the activities of the aerobes are confined to a shallower soil layer than in coarser grained soils. The reverse is true of anaerobic species. Methods of soil treatment tending to improve soil ventilation react both on the amount of chemical change produced by definite species, as well as the numerical ratio of different species to one another. Among such methods may be included drainage, liming, manuring and tillage. RATE OF OXIDATION or CARBON, HYDROGEN AND NITROGEN. Ex- periments carried out by Wollny proved conclusively that the production of carbon dioxide in soils is directly affected by the amount of oxygen supplied; that is, by the more or less thorough aeration of the soil. In one of these experiments air containing varying proportions of oxygen and nitrogen was passed through columns of soil. When this air contained 21 per cent of oxygen there were produced for every 1000 volumes of air 12.51 volumes of carbon dioxide; while with 2 per cent of oxygen in the entering air there were produced only 3.62 volumes of carbon dioxide. Similar observations were made by Schloesing in connection with the formation of carbon dioxide and of nitric acid. Deherain and many others have recorded the favorable influence of aeration on the rate of nitrate formation, while Lipman and Koch have observed an increased fixation of nitrogen by Azotobacter, consequent upon a better supply of oxygen. THE MINERALIZATION OF ORGANIC MATTER. Conditions that favor the intense activities of decay bacteria lead to a relatively rapid restora- tion of the phosphorus, sulphur, calcium, magnesium and potassium that had been made fast in plant tissues, to the stock of available plant food in the soil; indeed, in extremely well aerated soils the decomposition of or- 232 MICROBIOLOGY OF SOIL. ganic matter and its ultimate mineralization proceed too fast. It often happens that the farmer is unable to maintain a proper supply of humus in these soils because of their openness and is forced to adopt measures that will retard soil aeration. He resorts therefore, to rolling, marling, manuring and green manuring. On the other hand, heavy, fine-grained soils are not sufficiently well aerated to allow a rapid mineralization of the organic matter. Under extreme conditions the decomposition processes do not keep pace with the process making toward the accumulation of organic matter, and a more or less considerable increase in the amount of the latter takes place. This occurs in low lying meadows, and, more particularly, in bogs and swamps. Hence the farmer attempts to intensify aeration and the resulting mineralization of the humus by more thorough tillage, drainage, liming and manuring. TEMPERATURE. INFLUENCE OF CLIMATE AND SEASON. An illustration of the differ- ences that may exist in the soil temperatures of different regions is given by a comparison of the mean temperatures of 1901 recorded at Moscow, Idaho, and New Brunswick, New Jersey. The soil temperatures were taken to a depth of 152 mm. (6 inches). Soil Temperature,* 1901. Jan. Feb. Mch. Apr. May June July Aug. Sept. Oct. Nov. Dec. Moscow, Idaho 32 30 35 40 52 S8 68 72 S7 So 40 34 New Brunswick, 3i.S 28.6 35-3 47 57-9 72.1 76.4 73 .4 68.5 56.0 41.1 33.4 N. J. Air Temperatures* 1901. Moscow, Idaho 30 30.5 38.3 44.0 56.9 55-0 65.5 69.6 50.3 50.5 39-5 39-0 New Brunswick, 30.8 24.8 39-1 48.3 59- 2 70.9 77-4 74-6 67.6 54-6 38.6 32.6 N. J. *Recorded in Fahrenheit scale. It will be observed that in the months of November to March the soil temperatures in the two places were nearly the same. On the other hand, in April to October the average temperatures at New Brunswick were for soil 14.5 (58 F.) and for air 22.5 (72 F.), respectively; and in July MICROORGANISMS AS A FACTOR IN SOIL FERTILITY. 233 they were 20.0 (68 F.) and 24.5 (76.4 F.) respectively. It will also be observed that there is an unmistakable relation between the corre- sponding air and soil temperatures. As a further illustration of the relation of climate to temperature a comparison may be made of the average daily mean temperatures at Bismarck, North Dakota, for the period 1873-1895. and at Key West, Florida, for the period 1872-1895. Daily Mean Temperatures* (Air). Jan. Feb. Mch. Apr. May June July Aug. Sept. Oct. Nov. Dec. Bismarck, N. D. 4.5 9.5 22 .6 42.1 54. 2 63.8 69.5 67-5 S7.o 43.8 25-9 14-7 Key West, Fla. 69.7 7i .4 72.7 76.1 79-4 82.5 83.9 83-9 82.5 78.5 74-2 70.0 *Recorded in Fahrenheit scale. It is obvious from the figures given here that, because of the important temperature variations of different soil regions, the microbiological activi- ties must be profoundly modified. But apart from the climatic variations already indicated there are seasonal variations in any particular locality that are of great moment for soil microbiological activities. Such differ- ences are demonstrated by the temperatures of 1898 and 1902, taken to a depth of 152 mm. (6 inches), at New Brunswick, N. J. Soil Temperatures.* Jan. Feb. Mch. Apr. May June July Aug. Sept Oct. Nov. Dec. New Brunswick, N J. (1898). 33-2 33-1 45-1 48.9 59-1 76.0 79-3 77-8 72.0 60. i 44-6 33-6 New Brunswick N. J. (1902). 30.7 28.9 41-3 49-5 60.4 68.0 72 .6 70.5 65-9 56.4 48.6 34-1 * Recorded in Fahrenheit scale. ' In this instance, the season of 1898 was not only earlier, but the tem- peratures of June to September were sufficiently higher to favor more intense bacterial growth and activity. EARLY AND LATE SOILS. Under any given climatic conditions the warming up of soils in the spring will depend on their chemical and mechanical composition, color, tillage and topography. Because of the 234 MICROBIOLOGY OF SOIL. high specific heat of water, fine-grained soils containing a relatively large amount of moisture will warm up more slowly than coarse-grained soils containing a relatively small amount of moisture. The differences in the specific heat of humus, sand, clay and chalk are less important, yet they introduce appreciable variations in the soil temperature according to the proportion of each present. The topography of the soil introduces a factor of some importance for it affects the inclination toward the sun's rays as well as the drainage conditions. Tillage operations are of con- siderable moment, since they influence the rate of evaporation, that is, the rate at which heat is lost from the soil by the transformation of liquid water into vapor. Finally the color of soils exerts an influence on their temperature in that it affects the absorption and reflection of heat. Taking all of the factors together, it is found that sandy soils and sandy loams are early soils, because they part readily with their excess of water. Clay soils and clay loams are, on the other hand, late soils; it means, therefore, that in the more open soils microbial activities become intense earlier in the spring. Market gardeners usually attempt to improve matters still further by the use of large quantities of readily fermentable manure that develops enough heat to raise slightly the soil temperature. PRODUCTION AND ASSIMILATION OF PLANT FOOD. It was already observed by Moller that slight amounts of carbon dioxide may be evolved from frozen soil. Kostychev could detect a considerable production of carbon dioxide at o-5. In a series of experiments carried out by Wollny the amounts of carbon dioxide produced were as follows: COi in 1000 Vols. of Air. Water in Soil 10 20 30 4 S 6.79 per cent 2 O3 ^ 22 6 86 IA 60 2< 17 26.79 per cent . . . 18 38 CA 22 6^ so 80 06 81 52 46 79 per cent 2 c o7 82 12 91 86 The increased production of carbon dioxide at the higher temperatures, as shown in the above table, correspond with the observations that had already been made by Ebermayer, Schloesing and others, that carbon dioxide production in the soil is greater in summer than it is in winter. These facts, taken together with the early observations of Forster on the multiplication of photo-bacteria at o, and the more recent observations MICROORGANISMS AS A FACTOR IN SOIL FERTILITY. 235 of numerous investigators on the multiplication of individual species, or of mixtures of species in milk, water, soil, butter, etc., at o, or even below that, make it evident that bacterial activities are not entirely suspended at relatively low temperatures. As the latter rises these ac- tivities become more intense as gauged by the formation of carbon dioxide. Coming down to specific groups of soil bacteria, it may be noted that at 12 nitrification is already quite perceptible; that urea bacteria grow slowly at 5; Ps. radicicola at 4; members of the B. subtilis group at 6 10, etc. At 15 the breaking down of organic matter is fairly rapid, and at 25 the optimum is reached for many species. It follows, thus, that the production of plant food namely, ammonia, nitrates, sulphates, phosphates, etc. gains rapid headway as the optimum temperatures are approached. The organic matter itself, apart from serving as a source of plant food, furnishes carbon dioxide and various organic acids that help to attack the rock fragments and to render available compounds of phosphorus, potassium, calcium and magnesium. It is likewise evident that in warm countries bacterial activities are not only more intense at any one time, but they continue through a longer period. For this rea- son, the soils of the South can furnish both relatively and absolutely a greater amount of available plant food than the soils of the North. The production of plant food is necessarily followed by more vigorous growth of bacteria and of higher plants. More food is, therefore, assimi- lated and more moisture used up until the very rank growth of the crops hastens the depletion of the soil moisture. In this manner the soil may be dried out sufficiently to retard seriously the growth of soil bacteria and to retard thereby the decomposition of organic matter; under such conditions, moisture, rather than temperature, becomes the controlling factor of growth. REACTION. RANGE OF SOIL ACIDITY. Acid soils are very common in humid regions. The older soils of Europe include extensive areas whose lime content has been restored repeatedly by the application of wood ashes, marl, oyster and clam shells, and various grades of burned or crushed limestone. In the United States acidity is becoming prevalent in many of the cultivated soils, as is shown by the investigations of the Rhode Island, Ohio, Illinois, Oregon and Florida experiment stations. These investigations, confirmed by experiments in other states, show that there 236 MICROBIOLOGY OF SOIL. is a marked removal of lime and of other basic materials from the soil as cultivation and the use of commercial fertilizers become more thorough. Knisley shows, for instance, that 38.75 per cent of the Oregon soils ex- amined were acid, and that 16.25 per cent were strongly acid. Similarly, Blair found that of 189 soil samples of different Florida soils and subsoils, examined, 68.22 per cent of the former and 51.35 per cent of the latter were acid. He also found that virgin soils were less acid than cultivated soils. CAUSES OF SOIL ACIDITY. Soil acidity may be due to acids or acid salts, both inorganic and organic. ' Under ordinary conditions the latter are of much greater importance than the former as a cause of soil acidity. This is demonstrated by the extremely acid conditions of peat and muck soils that are particularly rich in organic acids. In soils left to themselves the formation of basic substances in the breaking down of silicates and other compounds keeps pace with their neutralization by acid and their removal in the drainage water. When soils are placed under cultivation, lime and other bases are removed more rapidly and the inert humic acids are left behind. The loss of bases is intensified by application of acid phosphate, potash salts and ammonium sulphate, commonly used as fertilizers. This accounts for the less extensive acidity in and among virgin soils as compared with cultivated soils. Arid soils lose scarcely any of their basic substances by leaching and are seldom acid. Residual limestone soils may be alkaline, neutral or acid, according to the loss of bases they have suffered by leaching. Low-lying soils, including meadows and swamps may accumulate large amounts of organic acids because of their imperfect aeration. EFFECT OF REACTION ON NUMBERS AND SPECIES. Some of the important groups of soil bacteria including nitro, azoto and ammonifying species will develop slowly or not at all, when the amount of acid in the medium is increased beyond a certain point. Hence it is realized by progressive farmers that a proper supply of lime is essential for the satis- factory decomposition of organic matter in the soil, and the abundant supply of available nitrogen compounds, as well as of other constituents of plant food to growing crops. The influence of lime on the multipli- cation of soil bacteria is well illustrated, for instance, by the experiments of Fabricius and von Feilitzen. These investigators found only 138,500 bacteria per g. in newly broken and unlimed peat soils; whereas in similar soils that had been limed and cultivated for several years the MICROORGANISMS AS A FACTOR IN SOIL FUTILITY. 237 numbers averaged about 7,000,000 per g. and reached a maximum of 22,132,000 per g. FOOD SUPPLY. ORGANIC MATTER. It may be said truly that a soil devoid of organic matter is practically devoid of bacteria. To the fresh and the partially decomposed organic matter (humus) the soil organisms must look for most of their food and energy. Being largely of plant origin this organic matter contains starches, fats, organic acids, higher alcohols, proteins and amino-compounds. Because of the different relations that these vege- table substances bear to the several species of soil bacteria, a high or low proportion of starch, of cellulose, or protein must necessarily modify both numbers and species relationships. For instance, observations have been made by Coleman and others that small amounts of dextrose favor nitrification, whereas larger quantities retard it; similarly, it has been noted that in the spontaneous decomposition of protein bodies bacteria are prominent and molds absent or relatively few in numbers. But where dextrose is added to the decomposing proteins molds soon appear in large numbers. There may also be cited, in this connection, the observations of Hilgard that humus should contain at least 4 per cent of nitrogen if it is to furnish a sufficient quantity of available nitrogen compounds; otherwise, the soil bacteria seem to be unable to decompose it, so as to meet the needs of the growing plants. Many similar facts could be cited to show that as a culture medium the soil is influenced by green manures, barnyard manure, commercial fertilizers, lime, tillage and any other treatment that will modify the quantity as well as the quality of its organic matter. THE MINERAL PORTION OF THE SOIL. The moisture films surround- ing the soil grains contain in solution substances derived from these soil grains. A particle of calcium carbonate will be surrounded by a moisture film containing some calcium bicarbonate. In the same way particles of feldspar may give rise to a solution of potassium bicarbonate; particles of apatite to a solution of calcium phosphate; particles of selenite to a solution of calcium sulphate; particles of protein to a solution of ammonia, etc. In view of the fact that these reactions are more or less localized and diffusion slow, there are, undoubtedly, in the soil minute zones where individual species are more prominent than they are in others. For example, Heinze has found it convenient to isolate Azotobacter by inocu 238 . MICROBIOLOGY OF SOIL. lating suitable culture solutions with particles of calcium carbonate picked out from the soil. Evidently these organisms were present in much greater abundance on these particles than on others of non-calcareous origin. Indeed, he occasionally obtained in this manner Azotobacter membranes that constituted almost pure cultures. The more general significance of this relation is apparent when it is remembered that nitro bacteria are particularly favored by magnesium carbonate; tubercle bacteria by gypsum and calcium carbonate; Azotobacter by cal- cium phosphate and calcium carbonate; photo-bacteria by sodium chloride, etc. Considerable as must be the local differences in any one soil, they are undoubtedly even more pronounced when different soils are compared. Extreme conditions are met with in certain irrigated soils in which a marked concentration of salts occurs. In so far as crop production is concerned, it is stated by Hilgard that the upper limit is practically reached when the concentration of soluble salts in the irrigation water is about 4-55 g- (7o gr.) per gallon. Nevertheless, in Egypt and the Sahara region irrigation water is occasionally used that contains more than 13 g. (200 gr.) of soluble salts per gallon. Further differences are introduced by the quality of these salts, e.g., the proportion of sodium sulphate, magnesium sulphate, sodium chloride, sodium carbonate, etc. Again, instances are on record, as in the investigations of Headden in Colorado and California, where the concentration of nitrates in the soil water is so great as to kill even relatively resistant plants like alfalfa. It is to be shown by future investigations what the effect of the concentration and composition of such salts may be on the soil bacteria. In humid soils conditions are less extreme, yet even here the variable concentration and composition of the soil solution are of direct moment for the different microorganisms. Granite soils, for instance, are fairly well supplied with phosphoric acid and abundantly with potash, but when hornblende is lacking they are apt to be deficient in lime. Ill- ventilated clay soils may contain reduction products of iron salts, while green sand, chalk, slate, shale, sandstone and other soils may have their individual peculiarities from the standpoint of a culture medium. BIOLOGICAL FACTORS. MOLDS. Soil bacteria must not only compete with other micro- organisms and higher plants for their food, but must contend with unf avor- MICROORGANISMS AS A FACTOR IN SOIL FERTILITY. 239 able changes caused in their medium by the competing organisms. In the case of molds a sufficient degree of acidity is often produced in the medium to retard or stop the growth of bacteria. This point is well illustrated by the prominent development of molds in culture solutions containing ammonium salts as the sole source of nitrogen. When the ammonium salts are replaced by nitrates under certain conditions the growth of molds is practically suppressed and bacteria come to the fore. In the soil itself the rapid development of molds has been observed in plots or pots receiving large additions of ammonium salts, a phenomenon due to the acid residues of the ammonium salts. The nitrates, on the other hand, give rise to alkaline residues since the "NO 3 " radical is used up in greater proportion than the basic radical. Similarly, molds are enabled to compete with bacteria when the proportion of sugar or of starch to protein is increased, or where large amounts of fats are present. ALG.E. At times the influence of algae in changing the character of the soil as a culture medium for bacteria is quite considerable. As chlorophyl-bearing organisms they are enabled to manufacture sugar and starch with the aid of sunlight, and favor thus the development of Azoto- bacter and of other microorganisms dependent for their energy on the organic matter in the soil. Investigators both in France and in Germany have found that the fixation of nitrogen in sand used for pot culture experiments occurs in the surface layer possessing a growth of algae. The advocates of bare fallows attribute the greater productivity of fallowed land to the growth of alga?, the accumulation of nitrogen by them and to other changes affecting the soil bacteria. PROTOZOA. It has been known for a long time that certain species of protozoa are common in soils and that their food consists of bacteria. To what extent protozoa play a part in soil fertility has not yet been fully explained, even though Russell and Hutchinson of the Rothamsted Experiment Station have maintained that these minute animals are extremely important in that they maintain a certain bacterial equilibrium in the soil. Their claim is mainly based on the fact that partially sterilized soils (either by means of heat or antiseptics) soon come to contain enor- mous numbers of bacteria. It is, therefore, assumed by them that this abnormal increase is made possible by the destruction of the protozoa that normally check the increase beyond a certain point. HIGHER PLANTS. Higher plants modify the soil as a culture medium for bacteria in at least three ways. The root-hairs come in contact with 240 MICROBIOLOGY OF SOIL. the moisture films surrounding the soil grains and not only modify the composition of the film water, by withdrawing a portion of the dissolved matter, but also change its character by secretions from the roots. The changes thus effected must, necessarily, modify the character of the soil and the soil solution as a culture medium. Again, the rapid removal of water from the soil by growing crops causes the film water to become more concentrated in so far, at least, as some salts are concerned. Modi- fications are, also, introduced thereby in the proportions of oxygen, nitrogen and carbon dioxide in the soil air. Finally, higher plants modify the soil environment for bacteria by their root and stubble residues. For example, residues of leguminous plants, being richer in nitrogen and possessing a narrower carbon-nitrogen ratio than the corresponding residues of non-legumes, will affect the soil somewhat differently than the latter. BACTERIA. Occupying, as they do, the leading role, bacteria demand a more detailed consideration, in fact, most of the biological discussions of soil are based upon a knowledge of these organisms. Numbers and Distribution; (Bacteria in Productive and Unproductive Soils] . Among the various factors that affect the numbers of bacteria in the soil moisture, aeration, food supply and reaction have already been discussed as important. Sandy soils because of their relative dryness and poverty in organic matter contain a comparatively small number of bac- teria, at times less than 100,000 and usually less than 1,000,000 per g. But when such sandy soils receive deep and thorough cultivation and are enriched in organic matter the numbers increase to several millions per g. In most loam soils in a good state of cultivation the numbers of bac- teria per g. range from about 1,000,000 to several millions. In heavy, compact soils the aeration conditions are unsatisfactory, acid substances and reduction products accumulate and the numbers are greatly reduced. Again, in peat and muck soils the numbers of bacteria are small when the reaction is markedly acid. It has been found that under such condi- tions the molds are more numerous than the bacteria and that the latter often occur to the extent of less than 100,000 per g. Generally speak- ing, the nigher the state of cultivation the greater the number of bacteria in the soil. It increases as we pass from forest and prairie to plowed fields, and from extensive field practice to intensive garden practice. Under special conditions, as in green-house soils generously supplied with manure and moisture, in sewage polluted soils, and in soils partly steri- MICROORGANISMS AS A FACTOR IN SOIL FERTILITY. 24! lized by heat or antiseptics the numbers may become enormous, 50,000,000 or even 100,000,000 per g. of material. Distribution at Different Depths. Most of the soil bacteria are found in the stratum in which the organic residues are concentrated, that is, in the surface soil. Immediately at the surface the rapid evaporation and the germicidal effect of direct sunshine act as disturbing factors, hence the numbers in the uppermost 25-50 mm. (1-2 in.) are smaller than in the layer of soil immediately below. Beyond the depth of 20 cm. or 22 cm. (8 or 9 in.) the numbers diminish rapidly. Material from a depth of .6 M. to .9 M. (2 to 3 ft.) is nearly sterile in humid regions. Differences occur, however, in keeping with the mechanical composition of the soil. In light, open soils the bacteria are not only carried down to greater depths by the percolating water, but can also multiply there, thanks to better aeration. On the contrary, fine-grained compact soils are more effective in holding back suspended material and do not allow the bacteria to pass downward as readily. Moreover, the less thorough aeration of these soils and the accumulation of toxic reduc- tion products in the subsoil serve as an effective check on the increase of bacteria in the deeper layers. In irrigated soils of the arid and semi-arid regions bacteria are dis- tributed at much greater depths. Their occurrence 2 M. to 3 M. (8 or 10 ft.) below the surface is made possible not only by the better aeration of these soils, but by the penetration of roots to great depths and the accumulation there of considerable amounts of organic matter. The practical significance of distribution appears, among other things, in the use of soil for inoculation purposes; for instance, it is reported by Sals- trom that in making peat soils arable the addition of small amounts of fertile loam increases to a very marked extent their crop-producing power. The efficiency of the inoculating material decreases as it is taken from the deeper soil layers. Similarly, in the use of alfalfa soil for the inoculation of new fields the most efficient material is secured at a depth between 7.62 cm. and 17.78 cm.( 3 and 7 in.). Morphological and Physiological Groups. (Morphological Groups). Rod-shaped organisms are numerically the most prominent among soil bacteria. They occur at times to the extent of 80 or 90 per cent of the total number. Spherical organisms usually constitute less than 25 per cent of the bacterial flora. Spirilla and Sarcinoe are present in slight numbers. Conditions may occur, however, when the proportion of 16 242 MICROBIOLOGY OF SOIL. spherical organisms is markedly increased. This happens, particularly, when large quantities of composted manure (rich in spherical organisms) is added to the soil. Among the rod-shaped species B. mycoides, B. stibtilis, B. mesentericus B. tumescens and other members of the subtilis group are quite prominent Members of the amylobacter group are seldom absent. Members of the proteus group and various fluorescents are always present, while Bact. arogenes and allied species are common inhabitants of the soil. (Physiological Groups}. In the decomposition of organic matter in the soil certain important changes in both nitrogenous and non-ni- trogenous material are accomplished by definite groups of bacteria. The breaking down of protein substances is accomplished by the formation of ammonia, nitrites and nitrates. These in turn may be transformed back into more complex amino- compounds, peptones, and proteins, or they may be destroyed with the evolution of free nitrogen. Moreover, there are groups of bacteria capable of joining non-nitrogenous organic matter to elementary nitrogen and of fashioning thus nitrogen compounds. Again, there are groups of bacteria bearing distinct and important relations to the decomposition of cellulose, or the transformation of its cleavage pro- ducts, methane and hydrogen. There are, likewise, definite groups of bacteria concerned in the transformation of sulphur and its compounds, and of ferrous compounds. METHODS OF STUDY. QUANTITATIVE RELATIONS. Since the early work of Koch in 1881 many investigators have determined the number of bacteria in soil samples, by means of the plate method. It is well known, however, that on ordinary gelatin or agar plates kept under aerobic conditions but a fraction of the soil organisms produce visible colonies. The anaerobic species do not appear, nor do aerobic Azotobacter, and nitro bacteria, while other common soil organisms form colonies sparingly or not at all. By employing synthetic agar media instead of beef broth gelatin or agar, Lipman and Brown have succeeded in securing the growth of a much larger number of colonies from any given quantity of soil, yet even these larger numbers were incomplete for reasons mentioned above. It is evident, therefore, that the results secured in the counting of soil bacteria have a relative value only. With the same media and methods MICROORGANISMS AS A FACTOR IN SOIL FERTILITY. 243 some information may be secured concerning the influence of fertilization, tillage, liming, etc., on certain of the soil bacteria. But even this infor- mation must be properly discounted, since equal numbers do not neces- sarily mean equal amounts of chemical work accomplished; for example, there is no certainty that 1,000,000 of decay bacteria derived from one soil will accomplish exactly as much decomposition as the same number of similar organisms from another soil. Otherwise stated, individual cells differ in their physiological efficiency from other cells of the same species. QUALITATIVE REACTIONS. By modifying the composition of the culture media different physiological groups may be favored in their development. In this manner the silica jelly medium proposed by Wino- gradski, or the gypsum plates proposed by Omelianski may be employed for making numerical comparisons of nitro bacteria in different soils. In like manner Beyerinck's mannit agar may be used for the numerical comparison of Azotobacter, and other media could be adapted for the quantitative-qualitative determination of urea, denitrifying, methane, and still other physiological groups of microorganisms. There is no doubt that the quantitative-qualitative method just out- lined may be made to yield valuable information. Yet it, too, possesses defects already noted in connection with the more strictly quantitative method. Apart from the vast amount of work involved in the prepa- ration of a large number of media and in the counting of colonies on many plates, this method fails to indicate differences in physiological efficiency. Furthermore, the colonies of the specific organisms sought are almost invariably accompanied by those of foreign species not always easily distinguished. With these limitations properly recognized and with further improvement in the make-up of special media the method may be made useful in supplementing data secured by other methods. TRANSFORMATION REACTIONS. Instead of counting soil bacteria in accordance with colonies produced in general or special media, soil investigators have attempted to measure the bacteriological functions of soils by comparing more or less definite quantities of the latter under known conditions. This method was employed by Wollny and others in studying the factors that affect the formation of carbon dioxide in soils. It was also used by Schloesing and Miintz and their followers in similar studies on nitrate formation. A method somewhat similar in principle but different in its application was proposed by Remy in 1902. He 244 MICROBIOLOGY OF SOIL. suggested the use of special media for the quantitative estimation of different physiological reactions; thus, making a i per cent solution of peptone and inoculating with equivalent quantities of soil, he caused the decomposition of the peptone and the formation of ammonia, and secured comparisons of the ammonifying power of different soils. In a similar manner he used special solutions for comparing quantitatively the trans- formation accomplished by nitrifying, denitrifying or nitrogen-fixing bacteria. Remy's method has been extensively tested by Lohnis, Ehrenberg, Lipman and others. It has been shown to possess a serious defect in that it deals with conditions unlike those occurring in the soil itself. For this reason more recent investigations have been carried on in weighed portions of soil rather than in culture solutions inoculated with 10 per cent of soil as is done in Remy's method. RATE or OXIDATION OF CARBON. The rate of decomposition of humus or of other organic matter in the soil may be measured, as was done by Wollny, by determining the amount of carbon dioxide evolved in weighed quantities of material kept under definite conditions. The influence of temperature, moisture, aeration, organic matter, antiseptics, etc., has been determined in this manner. The same method may be used in studying decay, and factors influencing decay, in soils in situ that is, in the field. More recently Russell and his associates have modified the method in that they have determined the rate of oxidation of carbon not by measuring the carbon dioxide evolved, but by estimating the amount of oxygen absorbed. In either case decay is measured from the carbon standpoint. The method based on this principle should find wide application in future soil fertility investigations. RATE OF OXIDATION OF NITROGEN. Another method or series of methods for studying decomposition processes in the soil may be based on the determination of nitrogen compounds formed in the breaking down of proteins. Two of the derivatives of protein, namely, ammonia and nitrate, have been used successfully to gauge the decomposition of organic matter in the soil. The recent results secured by Lipman and his associates demonstrate that ammonia formation from dried blood in weighed quantities of soil may serve as a very accurate measure of decay from the nitrogen standpoint. Corresponding determination of nitrates may similarly be employed in tracing protein cleavage and trans- MICROORGANISMS AS A FACTOR IN SOIL FERTILITY. 245 formation as influenced by the numerous factors of season, soil and cultivation. ADDITION OF NITROGEN. At least one other bacteriological factor in soils should be mentioned here as deserving attention in a systematic study of soil fertility from the nitrogen standpoint. It is known that Azo-bacteria are widely distributed in arable soils, and that they are more prominent in some regions than they are in others. The student of soil fertility finds it desirable, therefore, to study azotofication in different soils, and employs (for this purpose) mannit solutions like those proposed by Beyerinck, sand cultures supplied with sugar solutions like those proposed by Fischer, or weighed quantities of soil mixed with sugar as suggested by Koch. The methods referred to above make possible thus the study of ammonincation, nitrification and azotofication under controlled conditions and permit, thereby, the measure of bacteriological factors in soil fertility from the nitrogen standpoint. REACTIONS CONCERNING CALCIUM, MAGNESIUM, SULPHUR AND PHOSPHORUS. In addition to the purely chemical methods available for the study of these constituents, microbiological methods have also been suggested. In some of his still unpublished experiments with A zotobacter Lipman employed solutions of mannit in distilled water, provided with small quantities of sterile soil which were to supply the organisms with the essential mineral constituents. In this manner interesting data were secured on the availability of phosphorus compounds in different soils; similarly, Christensen has suggested the use of Azotobacter for determining the lime requirements of soils, and Butkevich has experimented with cultures of Aspcrgillus niger in determining the availability of the mineral constituents. CHAPTER II. THE DECOMPOSITION OF ORGANIC MATTER IN THE SOIL. CARBOHYDRATES ORIGIN. The sugars, starches, vegetable gums and allied pectine substances, as well as the cellulose, contained in roots and other crop residues add large quantities of carbohydrates to the soil. The crop residues are augmented still further by green manures and animal manures whenever these are used. A good growth of timothy, for example, may increase the content of organic matter in the surface soil by five hundred or a thousand pounds per acre, and three-quarters of this consists of carbohydrates. In the same manner, a green manure crop, or an application of barnyard manure may add to the land as much as fifteen hundred pounds, or even more, of carbohydrates per acre. These carbohydrates contain a large proportion of cellulose. THE DECOMPOSITION OF CELLULOSE. Pure cellulose (C 6 H 10 O 5 ) X is a rather inert substance, as exemplified by the resistance of cotton and flax fiber to decomposition processes. It is well known, nevertheless, that even cellulose is in the end decomposed and resolved into simple compounds. Plant roots, leaves and stems, as well as the trunks of fallen trees, gradually distintegrate and vanish. Under favorable con- ditions this may proceed rapidly, as is indicated by the processes in septic tanks, or in manure heaps on the one hand, and in open sandy soils on the other. The disappearance of cellulose may be accomplished by (a) anaerobic organisms, (b) by aerobic organisms, (c) by denitrifying bacteria, and (d) by molds. THE PRODUCTION or METHANE AND HYDROGEN. The decomposition of pure cellulose and the formation of methane and hydrogen mixed with other gases was first noted by Popov in 1875. Some years later Tappeiner and also Hoppe-Seyler confirmed Popov's observations that nearly pure cellulose in the form of Swedish filter-paper, or cotton fiber may be fer- mented by bacteria with the evolution of methane, carbon dioxide and occasionally also of hydrogen. These investigators ascribed the decom- 246 DECOMPOSITION OF ORGANIC MATTER IN THE SOIL. 247 position of cellulose to an organism found by Trdcul in decomposing vegetable materials, and named by him Amylobacter in 1865, because of the blue color assumed by it when stained with iodine. Subsequent investigations by Omelianski begun in 1894 and continued through a period of years demonstrated the presence of specific anaerobic organisms in decomposing cellulose. He described two distinct species of long, slender bacilli, assuming the clostridium form when in the spore stage. Morphologically the organisms can hardly be distinguished, but physiologically they show important differences in that one causes the fermentation of cellulose with the production of gases consisting of carbon dioxide and methane, while the gases produced by the other consist of carbon dioxide and hydrogen; hence the one is designated by Omelianski as the methane bacillus and the other the hydrogen bacillus. These organisms do not stain blue with iodine, and do not belong, therefore, to the butyric bacilli designated as Amylobacter by earlier investigators. Omelianski's investigations make it appear that the butyric organisms are not capable of fermenting cellulose proper. In culture solutions containing mineral salts and nitrogen in the form of ammonium compounds the decomposition of filter-paper and other forms of cellulose proceeds with considerable rapidity. Calcium carbon- ate must be added to neutralize the acids formed, otherwise the fermen- tation soon comes to a standstill. In one of Omelianski's experiments begun in October, 1895, and ended in November, 1896, 3.3471 g. of cellulose was decomposed by a nearly pure culture of hydrogen bacilli. The products consisted of 2.2402 g. fatty acids, 0.9722 g. carbon dioxide and 0.0138 g. of hydrogen, a total of 3.2262 g. which nearly accounts for all of the cellulose destroyed' The fatty acids were made up of butyric and acetic acids with a slight proportion of some higher homologue, probably valerianic acid. In a similar experiment with an apparently pure culture of the methane bacillus, begun in December, 1900, and ended in April, 1901, fermentation began after an incubation period of about one month, and the entire volume of gas gradually evolved was 552.2 c.c. This mixture consisted of 190.8 c.c. methane and 361.4 c.c. carbon dioxide. The products formed from the 2.0065 g- cellulose consumed included 1.0223 g- fatty acids, 0.8678 g. carbon dioxide and 0.1372 g. of methane, or a total of 2.0273 g. The slight difference in weight in favor of the fermen- tation products falls within the limit of error. These experiments show 248 MICROBIOLOGY OF SOIL. that about one half of the fermentation products is gaseous and that the other half consists of acetic and butyric acids. THE OXIDATION OF METHANE, HYDROGEN AND CARBON MON- OXIDE. Aside from cellulose, methane may also be produced from various other carbohydrates, organic acids and proteins. Large amounts of methane are thus contributed to the atmosphere by swamps, manure heaps and low-lying meadows. In a purely chemical way methane may also be set free from volcanoes and mineral springs. The constant additions of methane, ethane, hydrogen and carbon monoxide represent a considerable amount of potential energy. It is important to know, therefore, whether these materials are at all utilized. That methane may be utilized by bacteria as a source of energy was first shown by Sohngen in 1905. He isolated an organism named by him B. methanicus that showed itself capable of growing in inorganic solutions confined over an atmosphere of methane, oxygen and nitrogen. The methane gradually disappeared and there were formed consider- able quantities of organic matter. The ability to oxidize methane has been claimed for a number of other organisms by Sohngen and others. Early observations on the ability of moist soil to cause the oxidation of hydrogen are credited to de Saussure (1838). Many years later (1892) Immendorff called attention to the same fact. It was not, however, until 1905 that the oxidation of hydrogen was shown to be a specific biological process. In that year papers by Sohngen and Kaserer reported experi- ments wherein inorganic solutions confined under an atmosphere of hydro- gen, oxygen and carbon dioxide and inoculated with very small quantities of soil developed a bacterial membrane at the surface. The hydrogen was oxidized and organic matter produced at the expense of the energy set free. The observations just noted have been confirmed by other investigators, by means of mixtures and single species of soil bacteria. Finally it should be added here that B. oligocarbophilus previously isolated by Beyerinck and van Delden is able, according to Kaserer, to oxidize also carbon monoxide. THE CLEAVAGE AND FERMENTATION OF SUGARS, STARCHES AND GUMS. -Sugars are a very acceptable source of food and energy for soil bacteria. A culture solution containing suitable mineral salts and sugar ferments readily when inoculated with a small amount of fresh soil. When no combined nitrogen is added, Azotobacter, or B. (Clostridiuni) DECOMPOSITION OF ORGANIC MATTER IN THE SOIL. 249 pasteurianus (or both), may come to the fore. The cleavage products then include alcohols, organic acids and carbon dioxide. With B. (Clostridium) pasteurianus butyric acid is one of the prominent cleavage products. When combined nitrogen is also added to the culture solution other organisms will develop prominently, notably members of the subtilis group, butyric bacteria, aerogenes, etc. In the soil itself the addition of sugar leads to a very marked increase in num- ber and, if acid production is favored, molds may subsequently become prominent. In general it may be said that butyric, propionic, acetic, formic and lactic acid, and ethyl, propyl, butyl and iso-butyl alcohol are common cleavage products. In the case of starch, pectins and pentosans, similar conditions hold good. Diastatic enzymes seem to be produced by various bacteria, as well, as molds and streptothrices. Members of the subtilis group and B. fluorescens seem to be able to transform starch into sugar without difficulty. It needs hardly be added here that the vast quantities of organic acids and of carbon dioxide thus formed must play an important role in the breaking down of the mineral constituents in the soil. FATS AND WAXES. ORIGIN AND DECOMPOSITION. Plant substances contain varying proportions of fats and waxy materials. In the dry matter of grasses and cereal straw crude fat is usually present to the extent of 1.5 to 2.0 per cent. In hay made from clover and other legumes the proportion of crude fat is rather more than 2 per cent. In cereal grains it may range up to 4 or 5 per cent while in soy beans the content of crude fat is 19 per cent, in germ oil meal 22 per cent and flax seed meal 34 per cent. Under the influence of enzymes produced by molds, yeasts and bac- teria the fatty acids occurring as glycerides are decomposed into glycerin and fatty acids. The extent of fat decomposition, brought about largely by molds in the opinion of some, is shown by numerous experiments with peanut cake, olive press cake, cottonseed meal, almond oil, corn meal, etc. In a number of these experiments Aspergillus niger seemed to be particularly efficient in decomposing fats. Analogous decompo- sition processes may occur in the soil as proved by the experiments of Rubner. 250 MICROBIOLOGY OF SOIL. ORGANIC ACIDS. SOURCE. The cleavage products of proteins include large quantities of amino-acids. The latter are still further transformed and yield a variety of fatty acids. The carbohydrates being present in larger quan- tities than the proteins are still more important as a source of organic acids. Finally, the fats, gums, and higher alcohols contribute additional quantities of the latter. Among the more simple acids, acetic, propionic, butyric, oxalic, succinic and lactic are common. The extent of acid pro- duction was already indicated in connection with cellulose decomposition by the methane and hydrogen bacilli. Apart from these organisms, organic acids are formed by nearly every important species of soil bacteria; moreover, the tissues of dead plants and animals are not the sole source of organic acids in the soil. According to Stoklasa conditions may occa- sionally occur in the latter, especially when atmospheric oxygen is excluded, that favor the excretion by plant roots of appreciable quantities of acetic acid. TRANSFORMATION AND ACCUMULATION. Salts of organic acids are suitable as food for a wide range of soil bacteria. Azotobacter will readily make use of acetates, propionates and butyrates. A number of denitrifying bacteria will grow vigorously with citrates as the only source of organic nutrients. The fermentation of lactates by butyric bac- teria has been known for a long time. The decomposition of malates, succinates, tartrates and valerates may be accomplished by various species, and even simple compounds like formates may yield food and energy to certain soil bacteria, among them B. methylicus studied by Loew and his associates. It is evident, therefore, that organic acids are not liable to accumulate in well ventilated soils. Molds, as well as bacteria, destroy them rapidly, and carbonates, carbon dioxide and water are the final products of the decomposition of non-nitrogenous organic matter. Notwithstanding the ready decomposition of the more simple organic acids in the soil, it is well known that arable soils are frequently acid. This acidity is largely due to the so-called "humic acids," organic com- pounds whose composition is not well understood. They are composed, to some extent, of rather complex organic acids or of their acid salts. Continued cultivation seems to favor the accumulation of these acid compounds, partly on account of the diminished supply of lime and of other basic materials in older soils. When these soils are limed the DECOMPOSITION OF ORGANIC MATTER IN THE SOIL. 251 humic acids and acid humates are changed into neutral compounds and are then subject to more rapid decomposition by microorganisms. Ac- cording to the investigations of Blair the average acid soil in Florida requires 1,500 pounds of lime (CaO) per acre to neutralize the acidity to a depth of 84 mm. (9 in.). This means an acidity equivalent to more than one ton of hydrochloric acid per acre. In peat and muck soils the acidity is equivalent to many times this amount of hydrochloric acid. PROTEIN BODIES. AMOUNT AND QUALITY. The protein content of farm crops that leave residues in the soil is variable, but in all cases quite considerab e. Dried corn stalks contain 5 per cent of protein, timothy hay 6 per cent, red clover hay 12 per cent or more, alfalfa hay 15 or 16 per cent. Even wheat and rye straw may contain as much as 3 per cent of protein. Cotton seed meal and other oil cakes, -tankage, ground fish, hair and wool waste and dried blood (all used more or less extensively as sources of nitrogen to crops) are made up in a large measure of protein compounds. Being derived from plant residues, from microorganic, insect and animal remains, and from fertilizers and manures applied, the nitrogen in the soil humus exists, for the most part, in the form of protein com- pounds. Hilgard reports the following humus and nitrogen content, as based on the analyses of a large number of samples of humid, semi- arid and arid soils: (Humus) per cent (Nitrogen in humus) per cent (Nitrogen in soil) per cent Arid uplands O. 01 I ? 21 O 12 C Sub-irrigated arid soils i .06 * ^o 8 ?8 Wl X O^ Oooo Humid soils from humid and arid regions (California) 2 . A.Z ? 20 O T 3 C Humid soils from other states 7 OI o *y 1 78 u - MD o 20 z o / u ^* ^yo Taking the weight of an acre-foot of dry soil at 2,000,000 kg. (4,000,000 pounds) and multiplying the nitrogen by 6.25 (the factor usually employed for converting nitrogen into protein) we find the protein content of these soils to range from about 11,339 kg. (25,000 pounds) 252 MICROBIOLOGY OF SOIL. per acre to nearly three times as much. Similarly, the Illinois Ex- periment Station reports quantities of nitrogen equivalent to 3,175 to 4,989 kg. (7,000 to 11,000 pounds) per acre to a depth of 101.6 cm. (40 in.) in gray silt loams, of the lower Illinoisan glaciation. In the brown silt loams the amount of nitrogen to the same depth is usually more than 4,535 kg. (10,000 pounds) per acre; occasionally it is more than 9,071 kg. (20,000 pounds) per acre. In one instance a black clay loam of the late Wisconsin glaciation is reported to have about 13,154 kg. (29,000 pounds) of nitrogen per acre, to a depth of 101.6 cm. (40 in.). This would be equivalent to more than 81,646. kg. (180,000 pounds) of protein; of course, not all of the nitrogen in the soil exists in the form of protein, some of it occurring as amino-compounds, and a small por- tion as ammonia and nitrates. Nevertheless, by far the greatest part of it occurs as protein compounds. The protein compounds of the soil humus must be considered from the standpoint of quality as well as from the standpoint of quantity. It is well known that fresh plant residues are attacked more readily by micro- organisms than older plant substances. For this reason soils frequently supplied with fresh organic material supply greater amounts of available food to crops than similar soils whose organic matter consists, largely of older residues. CARBON-NITROGEN RATIO. The decomposition of organic matter is readily influenced by the relative content of nitrogenous and non-ni- trogenous compounds. Substances of animal origin yield relatively and absolutely more available nitrogen in a given length of time than sub- stances of plant origin. The difference noted is due largely to the greater proportion of protein in the animal materials; in other words, to the narrower carbon-nitrogen ratio. On this basis Hilgard attempts to explain the adequacy of the small proportion of humus in arid and semi- arid soils. Because of the narrower carbon-nitrogen ratio the humus compounds in these soils are decomposed with greater rapidity and yield a sufficient amount of ammonia and nitrate to supply the needs of the crop. But when plant substances alone are considered the statement just made requires qualification. It is true that cotton-seed meal or linseed meal, having a narrower carbon-nitrogen ratio, will decay more readily than corn-meal or wheat flour. It is also true that any given plant sub- stance, as it undergoes decay, will lose in proportion more carbon than DECOMPOSITION OF ORGANIC MATTER IN THE SOIL. 253 nitrogen. Older humus has, therefore, a narrower carbon-nitrogen ratio than humus of recent origin. It is likewise more resistant to decay than new humus. Hence under any given climatic conditions and in any given soil type, the carbon-nitrogen ratio may give important indi- cations as to the availability of the humus nitrogen. Lawes and Gilbert, as quoted by Hall, found the following carbon-nitrogen ratio in the organic matter of different soils: Cereal Roots and stubble 43 Leguminous stubble 23 Dung 1 8 Very old grass land 13 7 Manitoba prairie soils 13 Pasture recently laid down 11.7 Arable soil 10. i Clay subsoil 6 Hall concludes, therefore, that humus with a wide carbon-nitrogen ratio is more valuable than humus with a narrow carbon-nitrogen ratio, since it will be attacked more easily by the soil bacteria. THE TRANSFORMATION OF NITROGEN COMPOUNDS. AMMONIFICATION. Experimental Study. By ammonification is meant the production of ammonia by bacteria out of protein substances or their cleavage products. That ammonia production in the soil is a biological process was first demonstrated by Miintz and Coudon in 1893. These investigators showed that no ammpnia is formed in sterile soils. They also showed that ammonia may be produced out of nitrogenous organic matter by molds as well as by bacteria. Marchal not only confirmed these observations, but proved that various microogranisms differ markedly in their ability to produce ammonia. Of the several species of bacteria tested by him, B. mycoides (one of the common soil bacteria) proved itself particularly efficient in the breaking down of nitrogenous materials and the prodution of ammonia. Since the publication of these experiments a large number of investi- gators, both in Europe and America, have studied ammonia production in culture solutions as well as in the soil itself. It has been shown that under favorable conditions the breaking down of protein compounds and the formation of ammonia may be very rapid; for instance, in some ex- periments carried out by Lipman and his associates the following 254 MICROBIOLOGY OF SOIL. proportions of nitrogen were transformed into ammonia in the course of six days: Dried blood 16. 74 per cent. Concentrated tankage 56.66 per cent. Ground fish 47 . 16 per cent. Cottonseed meal 4- 95 P er cent - Bone meal 16. 65 per cent. Cow manure, solid and liquid excreta 32.60 per cent. Cow manure, solid excreta ... 5-39 P er cent - The experiments were carried out in equal quantities of soil and with equivalent quantities of nitrogen in the different substances. It will be observed that more than 56 per cent of the nitrogen in the concentrated tankage was transformed into ammonia, whereas under the same condi- tions cotton-seed meal yielded less than 5 per cent. Mechanism of Ammonia Production. The relatively large protein molecules are readily broken into larger or smaller fragments. This may be accomplished by purely chemical means, as, for instance, by boiling with acids or alkalies, or by biological activities. Among the first cleavage products albumoses and peptones are quite prominent. These in turn undergo further cleavage and the various amino-acids and their derivatives, as well as ammonia, make their appearance. In so far as the different species of bacteria are concerned, ammonia production seems to depend, to a marked extent, on the ability to secrete proteolytic enzymes. With the aid of such enzymes the proteins are more readily hydrolyzed and further changed into amino- and hydroxy acids and ammonia and carbon dioxide. Influence of Soil and Climatic Conditions. Ammonia production in the soil is affected by (a) its mechanical and chemical composition; by (b) the amount and distribution of rainfall; by (c) the prevailing temperatures; by (d) fertilizer treatment; and by (e) methods of tillage and cropping. The mechanical composition of the soil influences the proportion of aerobic and anaerobic species, while the chemical composition, particularly that of the humus, influences the rate of multiplication and the character of the chemical transformation accomplished. It is well known, for example, that additions of fresh organic matter intensify the rate of de- composition of the soil humus, and, likewise, ammonia production as was already demonstrated by Breal. In a more general way it was proved by Lipman and [his associates that, with a constant bacterial factor, DECOMPOSITION OF ORGANIC MATTER IN THE SOIL. 255 ammonia production in soils varies with the chemical and mechanical composition of the latter. In some of these experiments 100 g. portions of different soils were each mixed with 5 g. of dried blood, sterilized in the autoclave, cooled and inoculated with equal quantities of infusion from fresh soil. The following amounts of ammonia nitro- gen were produced in six days: Soil Ammonia nitrogen found A T. i . 62 mg. B 68. 20 mg. c 117.06 mg. D 107. 16 mg. E 1^6.47 ing. With all other factors constant, chemical and mechanical differences in the soil used were responsible for striking variations in ammonia production, as indicated by the figures given above. The influence of temperature and moisture conditions is fully as important as that of the chemical and mechanical composition of the soil. The following data secured by Lipman may be cited in this connection as showing the effect of moisture: One-hundred-gram quantities of air-dry soil were each mixed with 3 g. of dried blood and varying amounts of water added. The ammonia formed was distilled off and determined at the end of eight days. The amounts of ammonia nitrogen found were as follows: Water added Ammonia nitrogen found o c.c 4. IT, me. I C.C 4. 13 mg. ^ c.c. . =5.40 me. <; c c 10.64 mg. 7 c.c 26. T.7 mg. 10 c.c . . 40. S7 mg. 12 C C 70.71 mg. i e c.c o^.oo mg. 256 MICROBIOLOGY OF SOIL. It appears, therefore, that ammonia production in soils rises or falls as the rainfall or irrigation is increased or decreased, or as the soil water is more or less thoroughly conserved by proper methods of tillage. In the same way, seasons of high temperature favor ammonification while seasons of low temperatures discourage it. This point is well illustrated by the observations of Marchal that at o to 5 only traces of ammonia were formed in his culture solutions; that at 20 ammonia production was quite marked, and that at 30 the maximum was reached. Moreover, apart from the seasonal variations in any one locality, there is a wide range in ammonia production, as we pass from the torrid to the temperate and from the latter to the frigid zones. Species and Numbers. Ammonia production is a function common to most soil bacteria. Already in the earlier experiments of Marchal, 17 out of the 31 species tested were found capable of producing ammonia. Prominent among these ammonifiers were B. mycoides, B. (Proteus) vul- garis, B. mesentericus vulgattis, B. janthinus, and B. subtilis. Of a con- siderable number of soil bacteria tested by Chester all but one were ob- served to produce ammonia. In Gage 's experiments with sewage bacteria, 17 out of 20 species tested proved to be ammonifiers. Similarly, a num- ber of species tested by the writer, among them B. coli, B. cholerae suis, B. (Proteus) vulgaris, B. subtilis, B. tnegaterium, etc., all produced ammonia in meat infusions. A mass of additional data, accumulated by different investigators, furnish further proof that ammonia production is a common function of soil bacteria. The more prominent ammonifiers, including members of the B. subtilis group and certain Streptothrices, are numerically important in all arable soils. Their numbers are affected, however, by the amount and compo- sition of the soil humus. It has been found, for instance, that additions of straw and of strawy manure increase markedly the numbers of B. subtilis and of other members of the group. An increase in the numbers of certain ammonifiers is caused also by additions of lime or of green manure. For example, in experiments carried out by Lipman and his associates portions of fertile soil inoculated with B. mycoides were found to contain, a month later, 2,000,000 of bacteria per g. of soil. In similar soil portions that had also received additions of grass the num- ber was twice as great. Relative Efficiency of Different Species. In Marchal 's experiments already referred to, the species employed showed marked differences in their DECOMPOSITION OF ORGANIC MATTER IN THE SOIL. 257 ability to produce ammonia out of egg albumen. The following propor- tions of the protein nitrogen were converted into ammonia in twenty days: B. mycoides ............ 46 per cent. B. suUilis ................ 23 per cent. B. (Proteus') -vulgar is ... 36 per cent. B. janthinus ............... 23 per cent. B. mesentericus vulgatus. 29 per cent. B. fluorescens putidus ...... 22 per cent. Sarcina lutea .......... 27 per cent. B. fluorescens liquefaciens . . . 16 per cent. Furthermore, apart from the variations from species to species, differ- ences have been observed by Marchal and many other investigators between one strain and another of any single species isolated from the same or different soils. It must be remembered, therefore, that in the study of ammonincation in soils and culture solutions, due consideration should be given to differences in physiological efficiency as they are manifested by strains and species of microorganisms. Apart from the ammonifying bacteria already mentioned there is a group of organisms studied by Miiller, Pasteur, van Tieghem, Leube, Miquel, Beyerinck and others. These are the so-called urea bacteria, capable of intensive transformation of urea and allied compounds into ammonium carbonate, by means of the enzyme urease. NH 2 H 2 O=(NH 4 ) 2 CO 3 I NH 2 Morphologically these organisms include spherical and rod forms, spore-bearing and non-spore bearing species. Most of the urea bacteria are particularly prominent in the transformation of animal manures. NITRIFICATION. Experimental Study. The term nitrification refers to the oxidation either of ammonia or of nitrites to nitrates. In a broader sense nitrification may be defined as the production of nitrates from decomposing organic matter. Saltpeter or niter, the terms formerly applied to potassium nitrate, possessed, for a long time, a peculiar interest because of its relation to gunpowder. Whether it be true or not that gun- powder was known to the Chinese before the beginning of the present era, there is no doubt that for several centuries it played an important part in the political and economic history of Europe. The large quantities of gunpowder consumed in the almost incessant wars created a steady demand for saltpeter that was not readily met by the saltpeter refiners of India, Hungary and Poland. European nations, particularly France, 258 MICROBIOLOGY OF SOIL. were therefore thrown on their own resources and were forced to develop the domestic production of saltpeter. The industry came under govern- ment control and experts were appointed to study the so-called saltpeter plantations and the conditions affecting the appearance and increase of nitrates in compost heaps and in the soil. Much knowledge was thus gained about nitrification even though it was not suspected that living organisms were concerned in the process. With the rapid development of chemistry in the latter half of the eighteenth century a nearer approach was made to the understanding of the true character of nitrification. The observations of Cavendish in 1784 that potassium nitrate is formed when electric sparks are passed through air confined over a solution of potassium hydrate formed the starting-point for various theories that attempted to account for nitrate formation on the basis of purely chemical reactions. The formation of nitric acid and of its salts was thus assumed to be due to electric dis- charges in the atmosphere, to combustion processes in nature, or to the oxidation of organic matter and of calcium, magnesium iron and man- ganese compounds in the soil. Much credence was given to the latter explanation because of the almost universal occurrence of nitrates in arable soils. The first indication that nitrate production in the soil and in decaying organic matter is due to biological activities was first given by Pasteur in 1862. A few years later Miiller expressed his belief in the biological origin of nitrates and nitrites in sewage and drinking water. It was not, however, until 1877 that the true character of nitrification was made clear. In that year Schloesing and Miintz demonstrated that dilute solutions of ammonia could be changed into nitrate by being passed slowly through long tubes filled with soil. The amounts of nitrate nitrogen found in the leachings corresponded almost exactly to the amount of ammonia nitrogen used up. When the soil in the tubes was first sterilized by heating or by means of chloroform and other germi- cides, the ammonia passed through unchanged. But when soils ster- ilized by heat or chloroform were reinfected with small quantities of fresh soils nitrification again proceeded in a normal manner. The biological nature of nitrification having been thus established numerous investigators tried to isolate the specific organisms in pure culture. A large amount of work in this direction was done by Schloesing and Miintz, Celli and Marino-Zuco, Munro, Warington, the Franklands DECOMPOSITION OF ORGANIC MATTER IN THE SOIL. 259 and many others. A large number of bacteria, yeasts and molds were tested with negative results. Warington, who gathered a great mass of valuable information about nitrification, almost succeeded in securing pure cultures of nitrifying bacteria. Finally, Winogradski showed in 1890 not only that nitrification is caused by specific bacteria, but explained also why the others failed in securing pure cultures. He proved that these organisms do not develop colonies on the ordinary gelatin and other organic media, a fact whose recognition was largely responsible for his successful solution of the problem. The medium subsequently employed by him consisted of silicate jelly properly supplied with inorganic nutrient salts. After him other investigators proved that agar, deprived of its soluble organic matter, gypsum and sandstone disks, filter-paper pads, etc., could be used effectively as solid media. Nitrous and Nitric Bacteria. Winogradski's investigations led to the conclusion, foreshadowed by the earlier work of the Franklands and Warington, that the oxidation of ammonia proceeds in two stages, viz., (i) 2 NH 3 +3O 2 =2HNO 2 +2H 2 O ( 2 )2HNO 2 +O 2 =2HN0 3 The organisms oxidizing ammonia to nitrites, and designated as nitrous or nitrite bacteria, were called by Winogradski Nitrosomonas and Nitrosococcus. The former include species or varieties isolated from soils in Europe, Asia and Africa, and the latter those isolated from soils in America and Australia. The organisms oxidizing nitrites to nitrates and known as nitric or nitrate bacteria, were included by Wino- gradski in the genus Nitrobacter. Apart from these bacteria there is an organism, according to Kaserer, that can oxidize ammonia directly to nitrate. He named it B. nitrator. The reaction is illustrated by the following equation: NH 3 +H 2 CO 3 +O 2 =HNO 3 +H 2 O+CH 2 O-4i Cal. CH 2 O+O 2 =H 2 CO 3 -f-i32 Cal. Enough energy for the completion of the reaction is obtained by the oxidation of the formaldehyde (CH 2 O). Beyond the preliminary announcement of Kaserer's there are no experimental data to prove the existence of this organism, even though other evidence of an indirect nature may be construed to lend support to his theory. But whether it be proved or not that ammonia may be oxidized to nitrate by a single species, 260 MICROBIOLOGY OF SOIL. it is evident that the number of species concerned in nitrate production is relatively small. Relation to Environment. The conditions that affect nitrate formation in soils may be classified under the following heads: (a) supply of oxygen; (b) range of prevailing temperatures; (c) amount and distribution of moisture; (d) quantity of lime and of other basic materials; (e) quantity of soluble mineral salts; (f) character and amount of organic matter; (g) presence of toxic substances; (h) physiological efficiency of the nitrify- ing bacteria. The rapid disappearance of organic matter from sandy soils is due in large measure to their better aeration. On the other hand, the decom- position of vegetable and animal substances in heavy, ill-ventilated soils is materially retarded by the limited supply and very gradual renewal of oxygen. An intimate relation exists here between air and water in that the latter replaces the former to a more marked extent in heavy than in light soils. The influence of both aeration and the range of moisture is illustrated by an experiment of Lipman's in which equal quantities of soil were kept in large boxes under different moisture conditions. At the end of a year the following quantities of nitrate nitrogen were found: Moisture \ . > 6. 52 per cent 14.75 P er cent 18.62 per cent 22.05 percent 22. 12 per cent Nitrate nitrogen \ 697 mg. 823 mg. 720 mg. Trace Trace found In examining the figures recorded above, we find that moisture was the controlling factor in the development of the nitrifying bacteria, when the proportion of water in the soil was 6.52 per cent. As the amount of water increased to 14.75 P er cent there was a marked increase in the amount of nitrate produced. Beyond that, however, the further in- crease in the amount of water began to limit the supply of oxygen, and the production of nitrate nitrogen with 18.62 per cent of water in the soil was somewhat decreased. A still further addition of water up to 22.05 P er cen t l e d> practically, to saturation, and the encouragement of reduction rather than oxidation processes. Hence, no nitrate was al- lowed to accumulate in the soil. The data in question thus help to explain why care was taken, on saltpeter plantations, to keep the compost heaps moist, yet not too wet. DECOMPOSITION OF ORGANIC MATTER IN THE SOIL. 261 The influence of temperature on nitrate formation has been observed by many investigators. Already Schloesing and Miintz recorded that at 5 nitrification is quite feeble, at 12 marked and at 37 at its best. Other investigators have obtained substantially the same results, except that the optimum has been found to be considerably lower, often between 25 and 30. Under field conditions nitrification seems to take place at relatively low temperatures, as is indicated by the rapid oxidation of ammonium salts in the Rothamsted experiments in England; and the rapid decay and nitrification of clover and of other legume residues in the experiments at the New Jersey Experiment Station. These facts have, therefore, an important bearing on the nitrogen feeding of crops in tropical, subtropical and temperate zones. The influence of lime and of other basic substances including the carbonates of magnesium, potassium and sodium, and of the oxides of iron is of far-reaching importance in all nitrification processes. It is well known that applications of magnesian and non-magnesian lime, marl or wood ashes promote nitrification in the soil and in compost heaps, a fact that was well recognized by the ancient niter refiners. The favorable action of lime is readily explained by its ability to neutralise organic and mineral acids and to render, thereby, the soil reaction favorable for the rapid growth of ammonifying, as well as of nitrifying bacteria. Furthermore, the reserve of basic material serves to neutralize the acid formed by the bacteria and prevents thus the accumulation of an undue amount of acidity. The role of certain mineral salts in promoting nitrification is quite significant. Small amounts of sodium chloride have been found to favor nitrification in the experiments of Pichard and also those of Lipman. The former showed also that sulphates not only promote nitrification, but that different sulphates display marked variations in this respect. In the same manner nitrate formation was shown to be favorably affected by phosphates in bone meal, Thomas slag, and acid phosphates. Gener- ally speaking, therefore, nitrifying bacteria are stimulated in their de- velopment by a proper supply of available mineral nutrients. The exact relation of organic matter in the soil to the activities of nitrifying bacteria is but beginning to be properly understood. Earlier observations made it manifest that heavy applications of animal manures, or of green manure may not only retard nitrification, but may actually cause the disappearance of a part or of all of the nitrate in the soil. Sub- 262 MICROBIOLOGY OF SOIL. sequent experiments by Winogradski and by Winogradski and Ome- lianski showed that in pure cultures the presence of even slight amounts of soluble organic matter may depress or even suppress the development of the nitrifying bacteria. It was, therefore, concluded by these authors that relatively small amounts of soluble organic matter may inhibit nitrification. These conclusions, based on the study of liquid cultures only, were given a very broad application by many writers on agricultural topics. More recent experiments make it certain, however, that in the soil itself small amounts of soluble organic matter, e.g., dextrose, are not only harmless, but may really stimulate nitrification. It was shown, likewise, that humus and extracts of humus may, under suitable condi- tions, stimulate nitrification to a very striking extent. Certain substances in the soil may exert a toxic effect on nitrifying bacteria. Ferrous sulphate, sulphites and sulphides may thus act in- juriously, as may also calcium chloride and excessive concentrations of sodium carbonate, sodium bicarbonate, sodium chloride, magnesium sulphate, etc. Injury by ferrous compounds, as well as by organic acids, is not uncommon in low-lying fields and bogs; while injury from excessive concentration of soluble salts may occur in the so-called alkali lands. Finally nitrification in the soil should be considered from the stand- point of the organisms themselves. There is no doubt that continued growth under extremely favorable conditions leads to the development in the soil of nitrifying bacteria, possessing a very marked physiological effici- ency. On the other hand, in ill-aerated, sour soils the environment would depress the physiological efficiency of the nitrifying bacteria. Differences are thus undoubtedly established under actual field conditions, as is made probable by the variable behavior of soils from different sources when used as inoculating material in recently reclaimed or peat swamp lands. Accumulation and Disappearance of Nitrates. As shown above, the rate of formation of nitrates in the soil is dependent upon moisture, temperature and aeration, as well as on the presence of organic matter and basic substances. On the other hand, the accumulation of nitrates depends, under any given conditions, largely on the character of the growing crop. Observations on the rain gauges at Rothamsted showed an average annual loss 14 kg. (31.4 pounds) of nitric nitrogen per acre in the drainage water from uncropped soil. In one of King's experi- ments, land that had been fallowed contained 137 kg. (303.24 pounds) of nitric nitrogen per acre, to a depth of four feet. Adjoining cropped DECOMPOSITION OF ORGANIC MATTER IN THE SOIL. 263 land contained only 26 kg. (57.56 pounds) of nitric nitrogen per acre to the same depth. Stewart and Greaves found in limestone soil in Utah 64 kg. (142 pounds) of nitric nitrogen per acre, under corn; 98 pounds under potatoes, and only 12 kg. (27 pounds) under alfalfa. Under the same conditions fallow land contained 74 kg. (165 pounds) of nitric nitrogen per acre. The smaller amount of nitric nitrogen found under alfalfa bears out the observations already made by a number of other investigators that the accumulation of nitrates under legumes is smaller than it is under non-legumes. While several explanations have been offered to account for this fact, it is generally agreed that legumes assimilate nitrate nitrogen more rapidly than non-legumes. Unusual circumstances may favor, at times, the accumulation of quantities of nitrate large enough to destroy all vegetation. It is reported, for instance, by Headden that he has found in limited areas in Colorado as much as 9,0718.5 kg. (100 tons) of nitrate per acre foot of soil. The amount of nitrate nitrogen in the soil is influenced by the growing crop not alone because of the nitrogen absorbed by the latter, but because of the moisture relations as affected by growing plants. It is quite apparent that a large crop dries out the soil more rapidly than a small crop. When the soil moisture is sufficiently depleted, nitrification stops and the further accumulation of nitrates becomes impossible, while their disappearance is hastened by the constant demands of the crop. The disappearance of soil nitrates is, likewise, hastened by the leaching action of rain and by certain species of bacteria that transform them into other nitrogen compounds. DENITRIFICATION. Experimental Study. Denitrification may be de- fined as the reduction of nitrates by bacteria, involving the evolution of nitrogen gas or of nitrogen oxides. In a more general way, denitrification has been defined as the partial or complete reduction of nitrates by bacteria. The term direct denitrification has been suggested for complete reduction, and indirect for the partial reduction to nitrites or ammonia. The term denitrification should not be employed to designate losses of nitrogen gas due to the oxidation of ammonia, or to the disappearance of nitrates following their conversion into proteins by microorganisms. The reduction of nitrates in the presence of fermenting organic matter was noted by Kuhlmann as early as 1846. The same fact was recorded many years later by Froehde and by Angus Smith. In 1868 Schoenbein expressed the belief that nitrates may be reduced to nitrites by fungi. 264 MICROBIOLOGY OF SOIL. For more than a decade after that, data were rapidly accumulating in support of Schoenbein's contention, until in 1882 Gayon and Dupetit made it certain that nitrate reduction with the evolution of nitrogen gas may be caused by a "ferment." Finally, in 1886, the same investigators described two organisms, B. denilrificans a., and B. denilrificans /?., capable of completely reducing nitrates. Subsequently the studies of Giltay and Aberson, Burri and Stutzer, Severin, van Iterson, Jensen, Beyerinck and of many others not only greatly increased the number of known denitrifying bacteria, but added much to our knowledge con- cerning the development and activities of these organisms. It has been shown that a very large number of species can reduce nitrates to nitrites and ammonia; moreover, a considerable number of organisms are already known that can cause the complete destruction of nitrates with the evolu- tion of nitrogen gas or of nitrogefi oxides. The following reactions illus- trate diagrammatically the complete or partial reduction of nitrates. 2 HNO 3 =2HNO 2 +O 2 HN*O S +H 2 O=NH S +2O, 4 HNO 2 = 2H 2 O+ 2N 2 + 3 \ \ 1 \ \ \ \ \ \ 1 Pv \ 300 80 \ / 5 \ \ / \ 60 40 20 s, / i \ ^ \ 1 S \ / '\ * "S:^~. '^v - J C3 i V,v r:'^ : : ^-/ FIG. 86. Bacteria of slimy wine. A, B, C, pure cultures of various forms; D, muci- laginous sheath of slime bacteria. (After Kayser and Manceau.) Slime-forming Bacteria. -Musts and wines become slimy rarely through the action of Dematium pullulans (Wortmann) and wild yeast (Meisner) in the presence of oxygen but more frequently through the action of bacteria. In most cases only young wines after fermentation and when contained in closed casks or bottles exhibit this defect. A slimy wine has an oily appearance, pours without splashing and in extreme cases, becomes cloudy and will hang from a glass rod in strings. In such wines, the microscope reveals large numbers of almost spherical or more or less elongated bacteria in long chains. Other ob- MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 425 servers have noticed a diplococcus and a sarcina. Kayser and Manceau have recently investigated the subject very thoroughly and described a number of forms which are mostly short rods of from i/.< to 2/j. by .y/< to i.2/i. One large form, 3/z to^X i.6fj. to i.-j/n, was also noted. They all form chains, usually of considerable length. They all produce an abundant slimy sheath and stain easily with carbol-fuchsin and other aniline dyes and are Gram-positive (Fig. 86). These bacteria attack the sugar but neither the glycerin nor the alcohol and produce mannit, carbon dioxide, lactic and acetic acids and ethyl alcohol. The disease is usually not serious and disappears under the ordinary cellar treatment. Alcohol above thirteen per cent, free tartaric acid, tannin and sulphurous acid in small amounts prevent their growth. Propionic and Lactic Bacteria. The most serious and perhaps the commonest disease of wines is characterized by persistent cloudiness, disagreeable odors and flavors, increase of volatile acid and injury to or complete destruction of the color. Wines affected are characterized commonly as mousey, lactic or turned wines (Pousse and Tourne of the French) . The disease is due to bacteria. Enormous numbers are readily revealed by the microscope in badly affected wines. There seem to be several or many closely related forms, all short rod-shaped, isolated in the first stages of the disease, but later forming chains or filaments of various lengths. The most noticeable change caused in the composition of the wine is the decrease of fixed and increase of volatile acidity. The tartaric acid and tartrates are destroyed, and carbonic, acetic, lactic, propionic and other acids formed. Light wines of low acidity are most subject to this disease which may be prevented by measures which increase the acidity and alcohol, by rapid and complete defecation and attenuation of the wine with the proper use of sulphurous acid, and finally by timely filtration and pasteurization. Wines noticeably affected can be used only for distilling those badly affected are valueless. Mannitic Bacteria. Very sweet grapes of low acidity in hot climates are subject during fermentation to a similar trouble characterized by increase of volatile acidity and a persistent cloudiness and a vapid sweet- sour taste. The disease is commonly confused with the preceding but is caused by bacteria of different forms. The form described by Gayon 426 MICROBIOLOGY OF SPECIAL INDUSTRIES. is a very fine short rod which does not unite in filaments. It attacks the sugar, especially the levulose, producing volatile acids and mannit. The latter may reach over 2 per cent and the former 5 per cent, giving a sweet-sour wine which is completely spoiled. The bacteria grow abundantly only at high temperatures approaching 40 and can be controlled by cool fermentation, increase of acidity and proper use of sulphurous acid. Butyric Bacteria. In the cooler climates, wines, especially old red wines in bottles, often become bitter. This trouble is due to comparatively large rod-shaped bacteria, first described by Pasteur. The cells re- main united in angular filaments, short at first, but becoming longer and finally thicker with age by incrustations of coloring matter. s I \ /\ \ V 1 \w \ A } r \ / i> FIG. 87. Bacteria of wine diseases. A, bacteria of "turned wine," young wine (After Bioletti); B, bacteria of "turned wine," old wine (After Bioletti}; C, mannitic bacteria (After Maze and Pacottet); D, bacteria of "bitter wine" (After Pacottet). The tannin, coloring matter, and glycerin of the wine are attacked, acetic and butyric acids being formed. In small amounts the bacteria do little or no harm, in larger amounts they may spoil the wine. Means which increase the alcohol, tannin and acidity diminish the liability to the disease. Prompt attenuation and clarification and in extreme cases pasteurization will cure wines not too badly affected. All the above anaerobic bacteria of wine diseases probably exist in most wines. Which develop most, or whether any develop sufficiently to injure the wine depends on conditions, chiefly the composition of the must and the temperature at which the wine is fermented or stored. Most diseased wines show a mixed infection of several forms. MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 427 CONTROL OF THE MICROORGANISMS. Given grapes of suitable composition, the quality of the wine depends on the work of microorganisms. The art of the wine maker consists almost entirely in the control of these microorganisms. His success in facilitating the work of the useful form (true wine yeast) and in preventing or hindering the work of injurious forms determines the quality of his product. BEFORE FERMENTATION. On the skins of sound ripe grapes as they hang in the vineyard the microorganisms are comparatively few and in an inactive condition. With the utilization of intelligent methods they cannot injure the wine. On broken or injured grapes, the number is greater and the forms more active. If many such grapes occur they should not be mixed with the sound grapes if the best wine is to be made. Care should be taken to avoid unnecessary bruising of the fruit if it cannot be worked immediately. Molds, wild yeasts and acetic bacteria multiply rapidly on grapes wet with juice. The sooner the grapes can be crushed and placed in the fermenting vat or pressed the easier it is to obtain a sound fermentation. Cleanliness is essential. Grapes, which are gathered in moldy, vinegar-soured boxes, hauled in dirty wagons or cars, and passed through dirty crushers, conveyors and presses, may be so completely infected with injurious germs that it is impossible to obtain a good fermentation. The most injurious forms of dirt are must, grapes, or wine, which have been allowed to become moldy or vinegar-soured. Dust or soil is less injurious and, if excessive, may often be removed by sprink- ling, especially is this true if the grapes are too sweet and require dilution. Washing with antiseptics is not permissible. A weak solution of potassium metabisulphite might be used with benefit if it were not fop the difficulty of regulating the amount of sulphurous acid entering the fermenting vessel. If the grapes have to be kept for some time before crushing they should be kept as cool as possible to delay the growth of molds. Gathering in the cool of the morning is desirable and if grapes are gathered when warm they should be left in boxes to cool off during the night whenever possible. If the grapes are cool when they reach the fer- menting vat they will neutralize a certain proportion of the heat of fermentation, accordingly the difficulty of avoiding injuriously high temperatures is diminished. However carefully the grapes are handled, a certain amount of dust containing germs and other injurious matters will reach the vats and presses. In the manufacture of white wines, especially, it is desirable to get rid of these matters before fermentation. This is best accomplished by settling and decantation. As the juice runs from the press it is pumped into a settling tank or cask. If it is cold, below 1 5, and of full normal acidity, the impurities may settle in twenty to forty- eight hours. If the temperature is higher than 15 and the acidity low, molds and yeasts will develop or fermentation will start and prevent settling. A slight sulphuring with 428 MICROBIOLOGY OF SPECIAL INDUSTRIES. the fumes of burning sulphur or with a solution of potassium metabisulphite is there- fore usually necessary. The sulphuring should be as light as possible with acid musts as it tends to preserve the fixed acids. For the same reason it benefits musts of low acidity. In from twelve to twenty-four hours the must is purged of all its gross impuri- ties including microorganisms, dust and solid particles derived from the skins and the stems and pulp of the grapes. It may be slightly cloudy or nearly clear. It can then be drawn off into clean casks and fermentation started with yeast. This defecation is of great value, ridding the must of substances that would affect the flavor of the wine in the heat of fermentation and eliminating the excess of protein matters that would serve as food for injurious bacteria. Centrifugal machines have been devised to hasten the process of defecation, but their work is less perfect. Sterilization by heat has been tried for the same purpose but with indifferent success. High heating caramelizes part of the sugar and oxydizes the must, thus injuring the flavor. Discontinuous heating at lower temperatures in an atmosphere of carbon dioxide is preferable but troublesome and expensive; all methods have the defect of extracting undesirable substances from the solid matters which are heated with the must. Chemical sterilization is still less practicable. No substance could be used for this purpose except sulphur dioxide; this used in sufficient quantities would seriously injure the flavor of the wine. The effect would be totally different from that of the small quantities used in defecation. All the methods discussed have for their object the diminution or elimination of microorganisms of all kinds. With the injurious forms the true yeast is also removed. The more perfect these methods, the more necessary it is to add wine yeast. Without this addition, in fact, all these precautions may result in harm, for the wine yeast, being present in much smaller numbers than many of the injurious forms, may be completely removed while enough of other forms are left to spoil the wine. A "starter" of some kind is therefore necessary with defecated must and useful in all other cases. A Starter. One method of producing such a starter is to gather a suitable quantity of the cleanest and soundest ripe grapes in the vineyard, crush them carefully and allow them to undergo spontaneous fermentation. Perfectly ripe grapes should be selected and the fermentation allowed to proceed until at least 10 per cent of alcohol is pro- duced. If imperfectly ripened grapes are used or the starter used too soon, the principal yeast present will be S. apiculatus. Toward the end of the fermentation, 5. ellipsoideus pre-dominates. From 4 to 12 1. (i to 3 gallons) of this starter should be used for each 500 1. (100 gallons) of grapes or must to be fermented. Too much "starter" should not be used in hot weather or with warm grapes; unless this precau- tion is obesrved, it may be impossible to control the temperature. This starter is used only for the first vat or cask. Those following are started from the first fermentations, care being taken always to use the must only from a tank at the proper stage of fermentation and to avoid all tanks that show any defect. An improvement on a natural starter of this kind is a pure culture of tested yeast. MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 429 Such yeasts are being used extensively in Germany, France and Italy, usually with excellent results. The methods of use would require too much space to describe here, but they are simple and such as could easily be devised by anyone with some knowl- edge of microbiological technic. They do not aim at obtaining an absolutely pure fermentation, which is unnecessary, but endeavor to have an overwhelming proportion of a thoroughly tested and suitable yeast which will rapidly and perfectly attenuate the wine before the few injurious microorganisms present have time to do any harm. DURING FERMENTATION. However carefully the injurious germs have been excluded and the good yeast increased, fermentation will not be successful unless conditions as favorable to the latter and unfavorable to the former as possible are maintained. The temperature of the crushed grapes or expressed must is of importance. If it is below 15, unless the weather is warm, the grapes should be warmed to 20 or 25. Unless this is done, the molds and S. apiculatus, which require less heat than S. ellipsoideus will develop more quickly. This is especially true when starters are not used. In the warmer and earlier districts the grapes are practically never too cold. On the other hand, unless there is great carelessness, the grapes are never too warm for the commencement of fermentation. The warmer they are, however, the more artificial cooling will be necessary later, and the sooner it will have to be applied. Thorough crushing is necessary in the case of white wine, to facili- tate the expression of the juice. For red wine, the grapes are also thor- oughly crushed and the skin, pulp and juice are fermented together. Imperfectly crushed grapes ferment unevenly and incompletely; the growth of mold, is much facilitated. The must should be thoroughly saturated with air at the beginning of fermentation to insure the multiplication of the yeast. The aeration received in the processes of stemming, crushing and pressing is usually sufficient for this purpose. More aeration would be harmful by in- juring the flavor and color of the wine by over-oxidation and promoting the growth of injurious aerobic organisms. An objection to the sterili- zation of must by heat is the expulsion of the air and the difficulty of replacing it in the proper amount. The proper use of sulphurous acid in the regulation of fermenta- tion is one of the most important and necessary but least understood parts of the wine-maker's art. Only by this proper use can wholesome wine of the highest quality be produced. Improper use will injure 43 MICROBIOLOGY OF SPECIAL INDUSTRIES. or completely spoil the wine. Its beneficial effects are due primarily to its action on microorganisms, on enzymes and on the color of the wine. In the small quantities properly used in wine-making, it is antiseptic in a degree varying with the amount. All microorganisms are susceptible to its action in varying degrees. Bacteria are particularly sensitive, molds and pseudo-yeasts less so, while wine yeast is the most resistant of the ordinary forms found in must and wine. The result of the use of the proper amount of sulphurous acid in crushed grapes and must before fermentation is the almost complete suppression of bacterial action, the discouragement of molds and pseudo-yeasts and the promotion of the growth of wine yeast which is given a clear field unhindered by the deleterious excretions of competitors. Its action as regards enzymes is hardly less important. It would be impossible to make the finest wines of Sauternes and the Rheingau without its use on account of the oxidase produced by the Botrytis cinerea which is abundant and necessary on the best grapes of these regions. In other regions where this mold and others occasionally occur its use is also necessary. In hot climates it is especially useful, not only because bacterial action is more intense in such regions but because of its action in preserving the natural fixed acids of the grape, which are, there, nearly always deficient. This preservation, according to Wortmann, is due to the suppression of acid-consuming bacteria, but experiments of Astruc tend to show that the prevention of the action of unknown acid-destroying enzymes is in part the cause. Its action on the color of wines is also of importance. By the action of oxygen, the color of red wine is gradually made insoluble and precipitated, and the greenish or golden color of white wine is turned to brown. Both these actions are prevented or much diminished by the use of minute quantities of sulphurous acid. The most commonly used source of sulphurous acid is the fumes of burning sulphur. Sulphur is burned in a cask and the must caused to take up the fumes by being pumped into the cask through the upper bung hole. It is almost impracticable to apply sulphurous acid from this source to crushed grapes for red wine. The method is defective in many ways. It is impossible to tell within very wide limits how much sulphur dioxide has been absorbed by the wine. Moreover, the sulphur burns incompletely and the volatilized sulphur acted upon by the yeast may produce sulphuretted hydrogen. Other sulphur compounds are also produced during the burn- ing to some of which the so-called sulphur taste of wine is said to be due. Several devices have been invented to decrease these defects but none remove them completely and progressive wine-makers are adopting more reliable sources. An improvement is the use of potassium metabisulphite (K 2 S 2 O S ) a salt which can be obtained in the requisite purity in commerce containing 50 per cent by weight of sulphur dioxide. The amount of potash added by this salt in the doses used, is very small, and far within the limits of variation between different wines. By the use of this salt, exact amounts of sulphur dioxide can be applied both to white and red wines. Other sulphites are not permissible. The best source of the acid, recently brought into limited use, is the liquefied gas, which can be manufactured comparatively cheaply in great purity. By its use all the benefits of sulphurous acid are obtained and the defects eliminated. MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 431 Some grapes, owing to their composition, especially their high acidity, are very resistant to the attacks of injurious bacteria. Others, owing to their low acidity or highly nitrogenous nature, are very suscepti- ble. The addition of tartaric or citric acid to the latter has therefore a deterring effect on some of the most dangerous forms. It is seldom necessary, however, to modify the composition for this purpose if the other means of control are used. The addition of acid or its decrease by dilution should be solely for the direct improvement of the taste. The quality and character of the wine depends greatly on the tem- perature of fermentation. If too low, the fermentation may be unduly prolonged, the wine yeast may have difficulty in overcoming its com- petitors and the wine may remain inferior and cloudy. With red wine, the desired color, tannin and body may not be secured. On the other hand, if the temperature is too high the results are worse. The growth of bacteria is promoted, injuring the wine by the volatile acid and dis- pleasing flavors produced and preventing the proper action of the yeast. Such wines may remain sweet on account of the failure of the yeast to do its work and become unpleasantly acid owing to the volatile acids produced by the bacteria. Some means of controlling the temperature is therefore always needed. Where heat is deficient it may be supplied by direct heating of the must or part of it, or by heating the cellar. Where the heat is excessive, it may be diminished by crushing only cold grapes, using small fermenting vats to promote radiation and finally by the use of cooling machines applied directly to the fermenting wine. The best temperature for fermentation depends on the kind of wine. For light white wines, the maximum should not exceed 25, for heavier wines 30, while for heavy red wines where high extract and tannin are required, it may be allowed to reach 35. Sound wines can be made at all these temperatures. As already explained, the ordinary processes of treatment of grapes result in sufficient aeration for the multiplication of the yeast. With grapes containing little sugar, this may suffice to complete fermentation. With sweeter grapes, the fermentation usually slackens when the alcohol reaches n or 12 per cent by volume or sooner, unless some supplementary aeration is given. With white wine this is seldom done, with the result that the time of fermentation is prolonged. With red wine, the necessary stirring of the pomace to promote color extraction or the pumping over of 432 MICROBIOLOGY OF SPECIAL INDUSTRIES. the must in the cooling process usually gives a large amount of aeration which is sometimes excessive. Too much aeration results in extremely rapid fermentation and consequent difficulty in controlling the tempera- ture. It may also have a deleterious effect on the color, especially if sulphur dioxide has not been used. In any case, the main part of the fermentation should be over in from three to five days in the case of red and in from seven to fourteen days in the case of white wine. With heavy musts, however, there wall still remain from . 5 to i or 2 per cent of sugar. With certain special wines such as Sauternes it is desirable to retain the slight sweetness due to this small amount of unfermented sugar. This is accomplished by the judicious use of sulphurous acid, prompt clarification by filtration or fining and when necessary by pasteurization. The pasteurization tends to remove those proteins which are coagulated by heat and which are the preferred food of bacteria. In the case of dry wines, protection from bacteria is best obtained by prompt and complete attenuation. Fermentation should not be al- lowed to cease until all the sugar has disappeared. For this purpose, one, two or more aerations by pumping over are usually necessary im- mediately after the end of the tumultuous fermentation. The temperature of the wine should not be allowed to fall sufficiently to check the action of the yeast until all the sugar has disappeared. AFTER FERMENTATION. As soon as all the sugar has been destroyed, in the case of dry wines, or the desired degree of attenuation has been obtained in the case of sweet wines, all the useful work of microorganisms has been accomplished. The quality and safety of the wine then depend on freeing it from all organisms present and preventing the entrance and action of all others. As soon as bubbles of carbon dioxide cease to be given off, the yeast and other solid matters will settle to the bottom and the liquid become clear. This often occurs before the fermentation is complete. In this case the yeast should be stimulated by aeration as described above. If the wine is dry it should be racked (drawn off, decanted) from the sediment into clean casks. The first racking is usually done while the wine is still slightly cloudy during the first month or six weeks to remove the more bulky sediment. If left too long on the yeast the autophagy or degeneration of the latter may produce substances which injure the brightness and flavor of the wine. A second racking is necessary at the end of winter before the spring rise of tempera- MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 433 ture tends to renew the activity of the microorganisms which always remain in the wine. A well made wine at this time should be perfectly bright and all solid matters consisting of yeast and bacteria, coagulated proteins and crystals of bitartrate should have accumulated in the sediment. Racking should take place when possible only in settled weather, when the baro- metric pressure is high. Low atmospheric pressures diminish the solubility of the carbon dioxide with which the wine is saturated. Under these conditions, therefore, bubbles of gas are apt to be given off, bringing up particles of sediment and rendering the wine cloudy. However long wine is kept in wooden casks, it will continue to deposit sediment owing to chemical changes due to the action of oxygen which pene- trates slowly through the wood. Repeated rackings are therefore necessary, oc- curring at least twice a year until the wine is bottled or consumed. Abundant aeration is necessary during fermentation. A moderate supply of oxygen is necessary for the proper aging of wine. Experience has shown that exactly the proper amount of pure filtered air will obtain access to the wine for the latter pur- pose through the wood of ordinary casks of proper size. If the casks are too small the oxidation may be too rapid, if too large the maturing of the wine may be unduly pro- longed. The temperature of the storage cellar is the main modifying factor. The warmer the cellar the larger the casks should be. With sound, completely fermented wines, all aeration, other than that due to the porosity of the wood, should be avoided as much as possible. This is accomplished by keeping the casks tightly bunged and completely filled. Evaporation through the wood continually diminishes the volume of wine and the lack must be supplied by Jilting up, at first two or three times a month and later every month or two. The drier the air of the cellar, the more frequent the fillings necessary. A light sulphuring of the clean casks into which the wine is racked is usual. This should be practised with great caution. Very little is needed with sound wines, especially if it has been used before or during fermentation and a slight excess will injure the flavor. The amount should not exceed 1.25 g. per hectoliter for red or 2 g. for white wine. One-half to one-third of this is sufficient for old wines. The amount can be accurately measured only when using metabisulphite or the liquefied gas. The utility of the sulphur dioxide with perfectly sound wines is to dimin- ish oxidation; with wines liable to disease to discourage the growth of bacteria. All the manipulation of the wine should be conducted with strict attention to cleanliness. This applies especially to empty casks, pumps and hoses. These should be thoroughly cleaned immediately after use and, if of metal or other non-absorbent material, kept perfectly dry. Utensils of wood, rubber or other porous material should be preserved from bacterial or mold growth with sulphurous acid. The clarification of a perfectly sound wine may be facilitated and hastened by thoroughly stirring up the yeast immediately before racking. The yeast in settling carries down much of the finer suspended matter, thus effecting a rough fining. Mate- rials such as kaolin, pure silica sand, charcoal and filter-paper can be used with the same effect. The fining, however, is never perfect and the flavor of the wine is often injured. A very pure clay, known commercially as Spanish clay, is used largely for clearing sweet wines where the flavor is not so delicate. From 75 to 125 mg. per hectoliter are used for this purpose. 28 434 MICROBIOLOGY OF SPECIAL INDUSTRIES. The best wines are nearly always fined at least once, immediately before bottling. One or two finings may precede this to hasten aging, defecation and bottle ripeness. The materials used are soluble gelatinous or albuminous substances which are capable of being coagulated and precipitated by some ingredient of the wine. The best of the commonly used substances are Isinglas (Ichthyocol) 2 or 3 g. per hectoliter, for white wines; the white of fresh eggs, i or 2 per hectoliter for red ; and gelatin, i o or 1 2 g. per hectoliter for either. The proper quantity of the finings is dissolved in a little water diluted with wine and stirred into the cask. The tannins and acids of the wine cause a gradual coagula- tion in minute particles throughout the liquid. These particles gradually coalesce, forming larger particles which include all the other floating solid matter of the wine as in a net. These larger particles contracted by the alcohol then settle to the bottom, leaving the wine perfectly bright. The coagulum consists of a combination of the gelatinous matter and the tannin. Some of the latter, therefore, is removed from the wine. With astringent red wines this may be an improvement. If there is no excess of tannin present enough must be added to combine with the finings used. With white wines which contain little or no tannin this addition is always necessary. The amount to use varies with the quality of the finings and of the tannin and with the composition and temperature of the wine. To precipitate commercial gelatin of good quality about an equal quantity of good tannin is necessary; isinglas properly prepared requires only from one-half to one- third this amount. Eggs require only minute quantities. Specially prepared casein of milk is used for fining white wine. Its chief merit is that the acids of the wine alone cause its complete precipitation and no addition of tannin is needed. Many other albuminous substances such as milk, blood and various proprietary preparations are also used, but they are all inferior to the three mentioned and many of them introduce foreign matters such as milk sugar and bacteria which are a source of danger to the wine. Wines containing many disease-producing bacteria may be injured by the intro- duction of finings. The evolution of gases due to the bacterial action may prevent the settling and the protein matters introduced will favor the multiplication of the disease organisms. By the use of 5 to 10 g. of sulphurous acid per hectoliter added to the wine immediately before the addition of the gelatin, the bacteria may be temporarily para- lyzed and the finings will then settle and remove the bacteria with the other floating particles. The bright wine should be racked from the finings very soon after the sediment has settled, especially when disease-producing bacteria are numerous. This will be in from ten to twenty days. If the wine is not clear in three weeks it should be filtered. Filtering is inferior to fining in producing a perfectly bright wine. It is more rapid, however, and is useful in clearing common wine and wines refractory to fining. Filters of innumerable forms are used. They are of two main types. For rough clearing of very cloudy wines some form of bag filter is usually employed in which the wine passes through a cloth tissue. The passage at first is rapid and the filtration imperfect. As the solid matter accumulates on the filtering surface, the filtration im- proves but the passage of the wine is retarded. The first wine is passed a second time MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 435 through the filter and as soon as the rate of filtration becomes too slow the operation must be stopped and the filtering surface removed. For wines containing little sediment the filter must be primed. This is accom- plished by putting some finings in the wine first passed through the filter. The priming is more effective and the output of the filter much increased if a little in- fusorial earth is used with the gelatin. For the more perfect clearing of old wines some form of pulp filter is used. There are various devices by which the wine is forced through a mass of cellulose or asbestos pulp and freed from all floating matter. Some of the best of these, carefully used, remove nearly all of the bacteria present. BEER. Beer is an alcoholic beverage made from certain cereal grains by transformation of the starch to sugar, dilution with water, and fermenta- tion with yeast. There is usually an addition of hops and sometimes of materials containing sugar. The liquid before fermentation is called Wort. RAW MATERIALS AND MICROORGANISMS OF BREWING. GRAINS EMPLOYED. Barley, rice and maize are the grains most commonly used, wheat, rye and oats but rarely. Cane and beet sugars and syrups sometimes form part of the fermentable material. YEASTS OF BEER. The yeast used is usually one of the many forms of 5. cerevisicB. In some spontaneously fermented beer, other yeasts, Torulcc and bacteria take part, but in ordinary beers most of these are con- sidered as disease-producing organisms and injurious. KINDS OF BEER. The principal varieties of beer are : lager beers, fermented with bottom yeasts; ales, fermented with top yeasts (and Torulas); porters, similar to ale but dark in color owing to the use of caramelized malt; -weisbiers, in which lactic bacteria are abundant; and certain local types in which bacteria produce considerable quanti- ties of lactic and acetic acids. Typical Composition of Various Beers. Lager Ale Porter Weisbier Temper- ance beer Water OO AO 88 70 87 ?n Alcohol (by vol.) &. 8s 8 oo 7 J y 7 OO 3 A e 2f\f\ Extract 4 20 5e/i 6 A 45 Sugar. . i 60 54 T 1 1 45 I 87 u o T 7 T 95 T n8 Lactic acid 10 1 -66 2O 1.03 22 i.yj. 0*7 Ash 2? 3Q AQ */ 16 4 * J o H\j 436 MICROBIOLOGY OF SPECIAL INDUSTRIES. OUTLINE OF THE PROCESSES OF BREWING. INTRODUCTION. The manufacture of beer takes place in four main stages. First, a portion or all of the grain is soaked in water, allowed to germinate and then dried. This produces the malt which contains the enzymes necessary for the conversion of the starch into sugar and the disintegration of the tissues of the grain. The malt is then crushed (and usually mixed with unmalted cereals or sugar) and heated with water. This constitutes mashing. During this process, the starch changes to maltose and dextrins which with other matters dissolve in the water; then bacteria produce a small amount of lactic acid. The resulting solution constitutes the wort. The Wort, by the addition of yeast, is fermented and changed to beer. The fourth stage includes all manipulation of the fermented beer to prepare it for consump- tion. MALTING : PRODUCTION OF ENZYMES. The best malt is made from barley, but for special beers may be made from wheat or other grains. Steeping consists in soaking in water to start germination. This requires from thirty-six to seventy-two hours and causes an increase in weight of about 45 per cent. The temperature should be about 12.50. If higher, injurious molds will develop. If much lower germination will be retarded. The water should contain little organic matter or chlorides, nitrates or iron salts. A little calcium sulphate is favorable. If it contains many microorganisms it should be sterilized by boiling. A very little sulphite of lime or of potassium may be used to discourage molds. During germination several enzymes appear, of which the most important to the brewer are amylase which changes insoluble starch into soluble sugar, rendering it available for the growth of the young plant; peptase, which performs a similar function as regards nitrogenous matters; and cytase which helps in the disintegration of the cellu- lose. All these are necessary to prepare for the work of the yeast. When the plumule has grown to about two-thirds the length of the grain, sufficient enzymes have been formed. This requires from about sixteen to twenty days. The growth of the sprouting seed is at this point stopped by careful drying with artificial heat in a kiln. The kilning must be sufficiently rapid to kill the germinating seedling quickly, but not too rapid or at too high a temperature, otherwise the enzymes will be weakened or destroyed. The enzymes are more sensitive when moist, conse- quently the heat may be increased as drying proceeds. The process commencing at a temperature of 30 to 35 is increased gradually to 50 or 55. In twelve to twenty- four hours, the malt should appear dry. The temperature is again raised gradually for another twelve to twenty-four hours to 80 or 100. The lower the temperature the lighter the color of the malt. Higher temperatures, especially while the malt is moist, produce dark malt. As soon as the kilning is finished the radicles are removed by friction and screening in special machines. WORK or ENZYMES AND BACTERIA. The malt is first crushed by press- ing between rollers to facilitate the work of the enzymes and the dissolving action of the water. If unmalted grain is to be used as well, this must be ground and the starch made soluble by heating under pressure with three MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 437 or four times its weight of water and a little malt to 80 to 85 for about an hour. The methods of mashing are very various. They consist in general of mixing the ground malt with warm water, bringing the mass to a temperature of 35 to 45 which is gradually raised to 60 to 65 by the addition of hotter water. The action of the enzymes commences, the heated decoction of unmalted grains is added in various ways, and the temperature controlled by additions of hot water or by heating a portion of the mash. The whole mashing process requires from two to five hours according to the methods used. During the mashing the starch is transformed partly into maltose and partly into dextrins. The ratio of these products will vary according to the amount of amylase present and especially according to the temperature used. At about 60 the maximum amount of maltose is produced; at higher temperature (65 to 75) the unfermentable dextrins increase. The amount of alcohol and the amount of extract in the beer there- fore depend to a great extent on the method of mashing. During the first part of the mashing, while the temperature is about 45, lactic bacteria develop. If their action is too intense they will render the beer unpleasantly acid. If moderate, the acidity they com- municate to the wort is useful in preventing the growth of the harmful butyric bacteria which might develop. After mashing, the wort is separated from the solid matters by drawing off, extracting the mash with hot water (sparging), and nitration. It is then boiled from one to eight hours according to the result desired. Boiling sterilizes the wort, kills all bacteria and destroys any enzymes which remain. This occurs almost instantaneously owing to the lactic acid present. Coagulation of protein substances is also brought about, effecting a clarification of the wort. This requires one or more hours, according to the nature of the wort. It is necessary also in some cases to concentrate the wort, which is done by prolonged heating in open kettles. This may require several hours. The Hopping of the wort takes place during the boiling. Sometimes the hops are added just at the end of boiling; sometimes in two or three portions, one of which may be at the beginning and one after boiling. Hops contain an aromatic essential oil, resins and tannin. The essential oil is quickly soluble and volatile; to preserve its aroma in the beer, the hops must not be boiled too long. The resins are antiseptic and help to pre- serve the beer. They dissolve with more difficulty and require longer boiling. 438 MICROBIOLOGY OF SPECIAL INDUSTRIES. FERMENTAI ON: WORK OF YEAST. After boiling, the wort is separated from the hop debris by straining. It is then cooled by means of refrig- erators consisting usually of serpentine tubes through which cold brine or water runs. The hot wort runs or drips over the outside of these tubes in contact with the air. The final temperature of the wort is from 12 to 1 8 in top fermentation and 4 to 6 in bottom. By this means the wort is thoroughly aerated, which is necessary for the proper work of the yeast. It also effects a partial clarification by oxidation which causes a precipitation of solid matters. The fermentation takes place in two stages, the violent or tumultuous fermentation in vats and the secondary or after fermentation in casks. During the violent fermentation the temperature is allowed to reach a maximum of 7 to 9 with light beers, 8. 5 to 10.5 with dark and 12 to 20 in top fermentations. At the end of the first fermentation the beer is cooled gradually to 3.5 or 5.0 and drawn into fermenting casks where the after-fermentation takes place. The yeasts used in brewing vary very much. Besides the division into top and bottom yeasts, various types of each are recognized. One of the chief characteristics used for this division is expressed by the per- centage of the total extract fermented by the yeast. The Saaz type leaves all the dextrins and some of the maltose untouched and produces beers light in alcohol and high in extract. The Logos type destroys all the mal- tose and much of the dextrins. The result is high alcohol and low ex- tract. The Frohberg type is intermediate. These differences are prob- ably due to the differences in the amount and perhaps in the kinds of enzymes. The yeasts of spontaneously fermenting beers are of various species, S. ellipsoideus, S'. pasteuriamis and others. To produce fermentation, yeast is taken from previous vats so long as the yeast remains sufficiently uncontaminated with foreign organisms. The condition of the yeast is determined by the character of the fermen- tation, the degree of attenuation, and by microscopic examination. In breweries where modern pure culture methods are not used, the yeast present is always of several forms or types. In any case after a certain number of transfers, the yeast deteriorates and finally may become thoroughly infected with bacteria. The bacteria are revealed by microscopic examination. Where pure cultures are used, contamination with foreign yeasts is shown by a change in the time of MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 439 spore formation. By this method a contamination of i : 200 may be discovered. When the yeast becomes contaminated, a new start must be made with yeast from another brewery, which is uncertain, or by a starter of pure yeast, which is the only reliable method. The new start with pure yeast may be made by employing a kilogram of pure pressed yeast or a corresponding amount of liquid yeast and gradually increasing it to the desired amount by repeated small additions of sterile wort. This must be done with special precautions against contamination. Many large breweries use large pure yeast machines which produce directly sufficient yeast to start a fermenting vat. AFTER TREATMENT. The violent fermentation requires from eight to eighteen days according to the temperature. It takes place in open vats or sometimes, in top fermentation, in barrels. When sufficiently attenuated, the beer is drawn off into large casks where the slow second- ary fermentation takes place at a low temperature and the beer clears by depositing yeast and other sediment. The time required for the secondary fermentation is from six to ten weeks or, with certain types of beer, from two to four months or longer. A certain amount of dissolved carbonic acid is necessary for the quality and keeping of the beer. This is obtained by tightly bunging the casks at a suitable stage of the secondary fermentation. The clarification of the beer is sometimes assisted by placing a quantity of chips of beech or other tasteless wood in the casks. Top fermentation beers are often fined by the use of isinglas or animal gelatin. Low fermentation beers are usually filtered. The beer is then ready for delivery to the consumer and is placed in barrels with precautions to retain the dissolved carbonic acid. The clear beer may be put directly into bottles with the same precautions. Bot- tled beers which are to be kept for some time or which are to be shipped to a dis- tance are pasteurized after bottling at 60 to 65. DISEASES OF BEER. Beer may show defects due to imperfections in the raw material or in the methods of manufacture. These are principally abnormal flavors and lack of clearness. The diseases properly so called are due to wild yeasts or to bacteria. The disease-producing yeasts may be derived from the starter, from the vessels with which the beer comes in contact, or from the air. They 44 MICROBIOLOGY OF SPECIAL INDUSTRIES. develop most commonly during the secondary fermentation or in the bottle. Some may produce a disagreeable bitterness (S. pasteurianus I) or other unpleasant flavor (S. fcetidus) ; many produce a persistent cloudi- ness (S. ellipsoideus, S. apiculatus, S. exiguus, S. anomalus.} They are to be combated by preventing contamination, by proper attenuation and by pasteurizing. Bacterial diseases were more common before effective methods of purifying yeasts were known. Many forms of lactic bacteria may affect the beer, rendering it acid and cloudy. They occur principally where the temperature is allowed to become too high and where proper care in the cleaning and sterilization of utensils is not exercised. Acetic bacteria may occur under the same conditions and give a taste of vinegar to the beer. They are more common in top fermented beers. Various forms of Sarcina may cause persistent cloudiness, acid, un- pleasant flavors or both. This contamination may be from the air or water and is relatively common. The source of infection is to be looked for in the air or water. Their growth is most rapid at 16 to 20 and is retarded by the antiseptic properties of hops. Several kinds of bacteria, bacilli, cocci and sarcinas may cause the beer to become slimy or viscid and injure the flavor. This trouble is particularly common, in spontaneously fermented beer. Wort and beer, being organic solutions containing very little acidity, are favorable media for the growth of bacteria, many forms of which may cause trouble. With modern methods of using pure yeast, cleanli- ness and the pasteurization of bottle beer, diseases can be controlled. MISCELLANEOUS ALCOHOLIC BEVERAGES. CIDER AND PERRY. These beverages are made by the alcoholic fermentation of the juices of apples and pears respectively and come next to wine and beer in the quantities produced. The composition of the fruit varies very much according to the variety, especially in the matters of acidity, tannin and pectic substances. The following analysis is that of a good cider apple: Sugar 167 . o g. per liter. Tannin 2 . 4 g. per liter. Acidity (as sulphuric) : . i . 6 g. per liter. MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 441 The pectic matters vary from 2 g. to 25 g. per liter but should not be too high. Pears contain usually about the same amount of sugar as apples, more tannin and much less pectic substances. The microorganisms occurring naturally on the surface of the fruit are similar to those occurring on grapes, but special forms QiSaccharomyces are found. Pure cultures of wine yeast are used successfully in cider making where a perfectly dry cider is wanted. Where a small remnant of unfermented sugar is desired, the difficulties of using pure cultures have not yet been overcome. The wild yeasts occurring on the fruit in large quantities usually take precedence. Attempts to sterilize the juice by heating have not been successful owing to the production of a persistent cloudiness. It seems probable that a moderate use of sulphurous acid as in the case of wine may solve the difficulty. The principles of the control of the microorganisms, good and bad, are the same as in wine making. The same care in gathering and keeping the fruit and in extracting and handling the juice are necessary. The fermentation is similar to that of wine, but the cider should be taken off the yeast sooner in order to promote clarification and the re- tention of a little unfermented sugar. Cider is subject to the same bacterial alterations as wine and requires the same treatment. It is more difficult to keep when made in the ordi- nary way and is usually consumed during the first year. It is particularly subject to turning brown, owing to the large amount of oxidase present in apple juice. The use of sulphurous acid for preliminary defecation, pure yeast in the fermentation, and fining, followed by pasteurization soon after the fermentation, seem to offer the best means of improving present methods. FERMENTED BEVERAGES OF VARIOUS FRUITS. Many other fruits, especially those rich in sugar and with moderate acidity, are used locally to produce alcoholic beverages. The methods of fermentation are similar to those used in wine making, but additions of sugar and water are usually made to correct defects of composition. Very often distilled alcohol is also added after fermentation to preserve the liquid, which is thus rendered unsuitable for an ordinary beverage. 442 MICROBIOLOGY OF SPECIAL INDUSTRIES. HYDROMEL OR MEAD. An alcoholic beverage made by the fermentation of honey and water is much used in eastern Europe. Honey contains from 65 to 74 per cent of reducing sugars and from 2 to 10 per cent of saccharose. It is diluted with water to reduce its concentration to 22 Bal.* to 24 Bal. A few yeast cells are usually present in the honey but these are of various kinds and often unsuitable. The use of a good pure yeast is therefore advisable. As honey contains little mineral or nitrogenous yeast food, an addition of nutritive substances is necessary. The following formulae are recommended by Kayser and Boullanger to be used in one liter: A. Dicalcic phosphate i g. Ammonia 2 g. Bitartrate of potash 2 g. Magnesium sulphate o . i g. B. Maltopeptone i . 5 g. Bitartrate of potash i . 5 g. Ammonium phosphate i . o g. The same results may be obtained by mixing from 20 to 50 per cent of grape must or apple juice with the diluted honey. MISCELLANEOUS FERMENTED BEVERAGES. Fermented beverages of some kind are made in practically every part of the world. They are very numerous and varied but fall naturally into three groups; those made from the sweet juices of fruits or other plants in which the methods of manufacture resemble those of wine making; those made from starchy materials in which the methods resemble those of brew- ing; and finally those made from the milk of cows or other mammals which are discussed in Chapter IV, Div. IV. Belonging to the first group are numerous beverages made from the juices of sugar cane, various palms, and tropical fruits. The best known of these is the MEXICAN PULQUE made by the spontaneous fermentation of the sweet juice of the agave. Little is known about the microflora con- * "Balling" refers to the degrees of the special hydrometer for determining the specific gravity of saccharine solutions such as must or beer wort. Its purpose is to indicate directly the percentage of solids in solution at a temperature of 63.5 F. MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 443 cerned, but it includes alcohol-forming organisms which produce about 6 per cent of alcohol, and bacteria which cause rapid deterioration and spoiling of the fermented product. The pulque is ready for consumption twenty-four hours after the commencement of fermentation and cannot be kept more than a day or two. Of the beverages produced from starchy materials the Japanese SAKE, RICE BEER, has been most studied. It is made from rice by the diastatic action of Aspergillus oryzce and yeast fermentation. The process includes three stages. First the preparation of koji which consists of steamed rice on which the spores of the fungus are sown and allowed to grow at 20 until the whole mass is penetrated with mycelium. The next stage is the preparation of moto which is a thick liquid consisting of steamed rice, water and koji in which the fungus transforms the starch into sugar at o to 10 in a few days. Fermentation then starts sponta- neously, alcohol being produced by the action of several yeasts and lactic acid by bacteria, both present accidentally. In about two weeks the moto is ready. The last stage is the principal fermentation which occurs on mixing together steamed rice, koji, moto and water. This requires two weeks. The liquid is then separated, cleared and stored. It contains a considerable amount of alcohol and can be kept and aged like wine. POMBE is a kind of beer made in Africa from millet seed by sprouting to saccharify the starch and subsequent spontaneous fermentation in water. It is interesting as the source of the genus Schizosaccharomyces which appears to take the main part in the fermentation. GINGER BEER is an acid, slightly alcoholic beverage made by the fermentation of a 10 to 20 per cent solution of sugar containing a few pieces of ginger root. The fermentation is induced by adding small pieces of the so-called ginger-beer plant which consists of Bact. vermiforme and S. pyriformis. The bacteria form a thick gelatinous sheath and seems to live symbiotically with the yeast, each developing best in the presence of the other. DISTILLED ALCOHOL. INTRODUCTION. USES AND SOURCES OF ALCOHOL. Distilled alcohol is used as a beverage and a medicine or for innumerable purposes in the arts and industries. Certain methods and sources employed for the latter pur- poses are inadmissible for the former. 444 MICROBIOLOGY OF SPECIAL INDUSTRIES. In all cases, it is made by the preparation from saccharine or starchy substances of a sugar solution suitable for the work of yeast, the fer- mentation of this solution, and, finally, the distillation of the alcoholic liquid. Where the raw materials are sugary, methods similar to those of wine- making, and where starchy, to those of brewing, are employed, modified to suit the conditions of each case. The principal potable alcohols are brandy, made from grapes, rum from sugar cane, and whiskey from rye or other grains. Many other sources are used and any fermented beverage will, by distillation produce a potable spirit varying in character and quality with the source. In- dustrial alcohol may be made from any substance capable of undergoing alcoholic fermentation, the limiting factor in practice being, principally, the cost of the raw material per unit of alcohol. METHODS. PREPARATION OF THE SUGAR SOLUTION. Saccharine Raw Materials. When spirits are to be made from grapes or other fruit, the juice is fer- mented in the same way as for the corresponding beverage and then distilled. The juice, however, is diluted to 20 Bal. or less, as it is not necessary or desirable to have too much alcohol in the fermented liquid. The product is consumed directly as brandy or used to fortify sweet wines. The principal fruits used besides grapes are apples, peaches, plums and cherries. Industrial alcohol has been made from inferior or spoiled fruits and from cannery wastes, but the cost per unit of alcohol is usually high. The difficulties of fermentation are great, owing to the presence of large quantities of molds and other injurious organisms, and the extraction of the juice is troublesome. A careful use of sulphites and pure yeast simplify the process much. Sugar cane and its products are used in several ways to produce alcohol. To a limited extent the juice of the cane is fermented directly and distilled. The product is known as Jamaica rum. Much larger quantities of alcohol are manufactured from the cane-sugar molasses and appear in commerce as rum, tajfia, arrack or neutral spirits. For the making of Jamaica rum the juice is pressed from the crushed canes, and diluted with 20 per cent of vinasses (the residue of a previous distillation) to increase the acidity, and give the required flavor. MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 445 Cane molasses which contain from 50 to 60 per cent of fermentable sugar are diluted with water or vinasses to 15 to 18 Bal. and partially neutralized with lime when the acidity is excessive. One of the principal sources of industrial alcohol is the sugar beet. This alcohol is also used for the adulteration or imitation of potable spirits. It may be made by the direct fermentation of the beet juice, extracted by grinding and pressing, by methodical maceration or by diffusion. Sulphuric acid is added during extraction. This facilitates the extraction by setting free organic acids, and represses the growth of injurious microorganisms. The amount used should be such that a minute quantity of sulphuric acid remains free. Most beet alcohol is made from the coarser molasses of the sugar factories. The molasses are diluted to 20 to 30 Bal. with water, further diluted and heated with steam and acidified with sulphuric acid. The sulphuric acid neutralizes the lime which has been used in the manufacture of the sugar, sets free the volatile acids and breaks up the nitrites producing nitrogen peroxide. The liquid is then boiled for about one quarter of an hour to drive off the volatile acids and the oxides of nitrogen which would prevent yeast fermentation. The liquid after cooling is then fermented with yeast. Starchy Raw Materials. In the preparation of a fermentable solu- tion from starchy materials three methods for the conversion of the starch into sugar may be used, depending respectively on the action of malt, dilute mineral acids, and certain molds. The malt used in saccharification may be made in a manner similar to that described for brewing, from barley, oats, rye or maize. As the object in this case is to cause complete conversion of the starch with as little malt as possible, the malt should have the maximum diastatic power. For this reason, germination should be carried further than for brewing and the malt used green. Drying the malt destroys half its diastase. The conversion may also be accomplished by boiling one part of grain in four parts of water with hydrochloric or sulphuric acid. With the former acid, 10 per cent of the weight of the grain is used and 5 per cent with the latter. The conversion requires from eight to twelve hours' boiling. The starch is first converted into dextrins and then to glucose. If the boiling is too prolonged some of the glucose may be lost by conver- sion into caramel. The amount of acid and the time of boiling may be much reduced by operating under 2 to 3 kg. pressure. In this case 200 liters of water are heated with 100 kg. of grain and 4 kg. of acid. Conversion occurs in from 40 to 60 minutes. The power of certain molds, especially mucors, to convert starch into sugar has been utilized. Mucor rottxii found in Chinese yeast, Mucor oryzcB in Ragi, and related forms have been used for this purpose. This is known as the Amylo Process. The grain is first soaked for a few hours, then heated with twice its weight of water under a pressure of three and a half to four atmospheres until soft and the starch rendered soluble. 446 MICROBIOLOGY OF SPECIAL INDUSTRIES. The liquefaction of the starch is facilitated by slightly acidulating the water with hydrochloric acid. The mixture is then cooled to 38 and inoculated with a pure culture of the Mucor. A current of filtered air is then passed through the mass for twenty-four hours, by which time the mycelium has permeated the mass. The temperature is then reduced to 33, pure yeast added and aeration continued for twenty-four hours longer to promote the multiplication of the yeast. Conversion of the starch and fermentation of the sugar then continue together. The mucor is capable of fermenting the su^rtr and producing alcohol, but the yeast acts more rapidly. The malting process is the most commonly employed. The acid process destroys a greater part of the value of the residues of distillation and the amylo process, requiring costly special equipment and large expenditures for fuel, has not come into general use. The starchy substances used being usually neutral or of low acidity the sugar solu- tions produced would be very liable to bacterial invasion unless means of prevention were used. In the amylo process the sterilization of the solutions and the use of pure cultures accomplish this end. In the acid process the minute quan- tity of free mineral acid remaining in the completed solution prevents any considerable growth of bacteria. In the malting process the injurious bacteria are restrained by lactic acid produced by lactic bacteria, originat- ing in the malt or in the yeast starter. The requisite bacteria are obtained by keeping the starter or mother yeast at 50 to 58 for a certain time. This is a favorable temperature for lactic and too high for the develop- ment of acetic or other injurious bacteria. When the acidity of the solution reaches 3.5 g. to 5 g. per liter the dangerous butyric bacteria cannot develop. Pure lactic acid may be added immediately after saccharification and the loss of sugar, due to the action of the lactic bacteria avoided, but the high cost of the pure acid prevents the practice. Yeast being much less sensitive to the presence of certain antiseptics than bacteria it is possible to control the latter by the addition of suitable amounts of an antiseptic to the sugar solution. By gradually increasing the amount, moreover, yeast can be accustomed to amounts of antiseptics which render the growth of bacteria impossible. An application of this principle is found in the use of sulphurous acid in wine-making. In Effront's method for the preparation of distillation material, hydrofluoric acid is used. This acid is added to the mother yeast at the rate of 10 g. MICROBIOLOGY OF ALCOHOL AND ALCOHOLIC PRODUCTS. 447 per hectoliter and to the sugar solution in somewhat smaller amounts. This results in the inhibition of lactic, butyric and other bacteria and an increase in the fermentative power of the trained yeast. FERMENTATION. The sugar solution properly diluted and acetified or sterilized is fermented by the addition of a mother yeast, usually taken from a previous fermentation. The original yeast may be obtained by a spontaneous fermentation as is usual in the manufacture of rum. Such a yeast is always impure, containing various yeasts, molds and bacteria, and is therefore very variable and uncertain in its results. In the fermentation of beet juice and beet molasses, beer yeast of the Frohberg type or special distillers yeasts are used. A starter or mother yeast is prepared for each vat or the process is made continuous by leaving one-third to one-half of the contents of a fermented vat to start a fresh addition of the sugar solution. With the latter method the yeast in time becomes weak and badly contaminated and a new start must be made with fresh yeast. In the fermentation of solutions made from potatoes, corn or other starchy substances, each vat is started with a mother yeast. The tem- perature should be kept below 30 by means of refrigeration, otherwise alcohol will be lost by the multiplication of bacteria. By the use of pure yeast, the yield in alcohol is greater as no sugar is wasted in the production of lactic acid. The cost, however, is greater owing to the necessity of the use of more heat in sterilization. The fermentation of sugar-cane molasses for the production of arrack is brought about by the use of a mother yeast called tape], prepared from ragi or Java yeast. Tapej is made by mixing powdered ragi with boiled rice. In two days the rice is reduced to a semi-fluid condition and contains bacteria, molds and yeasts. The bacteria seem to have no part in the process but when too numerous are injurious. The mold Mucor oryza converts the rice starch into sugar and the yeast S. vordemanni produces alcohol from the sugar. The other molds present are more or less injurious. CHAPTER VII.* THE MANUFACTURE OF VINEGAR. ACETIC FERMENTATION. NATURE AND ORIGIN OF VINEGAR.- Vinegar is a condiment made from various sugary or starchy matters by alcoholic and subsequent acetic fermentation. It should contain from 4 to 8 per cent of acetic acid and natural flavoring, coloring and other matters, varying according to its origin. Acetic acid (CH 3 COOH) is a monobasic organic acid the second in the fatty acid series. It is a colorless liquid with a strong suffocating odor, crystalizing when pure at 16.7 and at lower temperatures when diluted with from i to 13 per cent of water. Its specific gravity is 1.08 at o and it boils at 118 under 760 mm. pressure, producing an inflam- mable vapor. It is a solvent of many organic substances and is soluble in water and alcohol in all proportions. The metallic acetates are poisonous and are formed in most cases by simple contact of metal and acid. Certain alloys of tin resist the action of the acid. Acetic acid is formed by the oxidation of ethyl alcohol which takes place in two stages according to the following reactions: C 2 H 6 0+ O =C 2 H 4 + H 2 O Ethyl + Oxygen = Acetic + Water, alcohol aldehyde C 2 H 4 0+ O =C 2 H 4 O 2 Acetic + Oxygen = Acetic acid, aldehyde These reactions may be brought about by chemical means, but in practice they are due to the action of certain microorganisms, mainly bacteria. Acetic acid is also made by the distillation of wood but the product is not suitable for consumption. VINEGAR BACTERIA. If wine, beer or a similar organic solution con- * Prepared by F. T. Bioletti. 448 THE MANUFACTURE OF VINEGAR. 449 taining alcohol, is exposed freely to the air, it soon becomes covered with a film, the alcohol disappears, is replaced by acetic acid and the liquid is converted into vinegar. This film, the Mycoderma aceti of Pasteur, consists of bacteria coher- ing by means of a glutinous sheath surrounding each cell, forming a zooglea. If the film is undisturbed, the liquid remains clear until converted into vinegar, if disturbed, portions may sink, new films form and finally a large gelatinous zoogleic mass, "the mother of vinegar," may form in the liquid. Sometimes, especially on liquids containing sugar and large amounts of alcohol, such as sweet wines, the film formed consists, not of bacteria, but of a yeast-like fungus, Mycoderma mni. Wines which have been sterilized, often remain without acetifying for a considerable time. Those containing traces of sulphurous acid acetify slowly and with difficulty. Ordinarily at warm temperatures, exposed wines develop a bacterial film very rapidly owing to the almost constant presence of some acetic bacteria in all wines. Hansen was the first to show that the vinegar bacteria included more than one species. He isolated and described three species concerned with the spontaneous souring of beers. Later it was shown by A. J. Brown, Henneberg and others that several other species commonly occurred in vinegar factories and that many more were capable of pro- ducing acetic acid in small amounts. The species which have been most thoroughly studied and which seem to occur most usually in vinegar factories are Bad. aceti, Bact, pasteurianum, Bad. kutzingianum, Bad.