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: 



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) 



