eChapter Name: Determination of Available Nitrogen in Soil [Alkaline Permanganate/Subbiah and Asija (1956) Method]
9789390591954
eBook Name: A PRACTICAL MANUAL ON GEOLOGY AND SOILS
by A. S. Mailappa
[Alkaline Permanganate / Subbiah and Asija (1956) Method]
Introduction
Nitrogen (N) is found in the arable horizon of the soil, mostly in organic material. In the soil solution, organic N is gradually transformed into ammoniacal (NH4 +), nitrite (NO2 –) and nitrate (NO3 –) nitrogen by microbial processes. Organic-N is, in itself, of very little use to plants, as it can not be absorbed as such. It is, therefore, necessary to estimate the different forms of mineralized or available N. The NO3 –_N and NO2 –-N together, hardly, exceed 1 % of the total N in normal soil.
The available N in soil refers to a fraction of the total N which is converted into forms accessible to the plants. This constitutes, on an average, only 0.5-2.5 % (rarely 5 %) of the total N in a soil at any given time. Nitrogen is, generally, absorbed by plants as NO3 –, under oxidized environment (upland condition), and as NH4 +, under reduced condition. NO2 – is sometimes, detectable, but the amount is, generally, very small vis-a-vis NH4 + or NO3 – and, hence does not warrant its determination. The sum total of NH4 + and NO3 –- N is smaller than the total N, which becomes available to plants and the difference being attributed to the mineralization of the organic N, during the crop growth cycle.