378 PHYSIOLOGY 



it) be composed chiefly of proteins (probably more complex and labile 

 than in the non-living state), it is evident thai protein foods are of the 

 highest importance — indeed indispensable — for nutrition, since it is 

 the protoplasm which grows, wastes, and needs repair. Proteins are, 

 as it were, the highest type of foods; they represent the final stage of 

 food making. 



Inasmuch as the carbohydrates contain only carbon, hydrogen, and 

 oxygen, while proteins contain in addition nitrogen and sulfur and in 

 many cases phosphorus also, it is plain that they cannot be formed from 

 carbohydrates alone. A strict carbohydrate diet is as unsuitable for 

 plants as it is for animals. Some materials must be supplied from which 

 nitrogen, sulfur, and phosphorus can be obtained. 



Source of nitrogen. — As the air contains 78 per cent of nitrogen, the 

 atmosphere would appear to be a natural source of this element. But 

 though the nitrogen is everywhere dissolved in the water of the plant, 

 and can enter and leave it freely, no plants are known to be able to use 

 it in this uncombined form, except certain bacteria, some of which live 

 in the soil and in some waters. Certain soil species enter the roots of 

 various plants, especially the Leguminosae, causing them to form tuber- 

 cles. (See below, p. 379.) Almost all plants, therefore, must get com- 

 bined nitrogen. This is found in soils as nitrates of various bases, e.g. 

 calcium, magnesium, potassium, and sodium; and when a soil is deficient 

 in nitrogen, such compounds are important constituents of the fertilizers, 

 natural and artificial, which are added to it. The nitrates in the soil 

 result mainly from the decay of organic matter in it. The later steps 

 in the process are controlled by certain bacteria in the soil which bring 

 about the oxidation of ammonia to nitrites, whereupon others oxidize 

 the nitrites to nitrates. The very fertility of arable soils, therefore, 

 depends on the microscopic organisms living in them, which prepare the 

 way for the larger plants. 



Loss of N. — The soil of cultivated areas is constantly losing its com- 

 bined nitrogen by solution and drainage, and this loss is only partially 

 made good by the ammonia and nitrous and nitric acids washed into it 

 from the air by rains. Under natural conditions the dying vegetation 

 ultimately returns its constituents to soil and air ; but crops are carried 

 off, their nitrogen with them. Gardens and fields, therefore, require 

 replacement of this nitrogen sooner or later. When they lie fallow, 

 certain bacteria of the soil, associated with algae and perhaps with 

 other plants, slowly increase the nitrogen content of the soil by fixing 



