374 MICROBIOLOGY OF SOIL 



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 

 transformation as influenced by the various 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 solu- 

 tions 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 

 ammonification, nitrification and azotofication under controlled con- 

 ditions 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 In some of his still unpublished experiments with A zoto- 

 bacter Lipman employed solutions of mannit in distilled water, provided 

 with small quantities of sterile soils 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 Azoto- 

 bader for determining the lime requirements of soils, and Butkevich 

 has experimented with cultures of Aspergillus niger in determining the 

 availability of the mineral constituents. 



