The chemical study of submerged soil is of great importance and its practical significance hardly needs any emphasis. Much work has been done on the decomposition of green manure in paddy soils (Acharya, 1935; Tenny Waksman, 1930 and Harrison and Aiyer, 1916). However, the N regime under water-logged condition characteristic of the virtual absence of nitrates and accumulation of ammoniacal N has not been fully worked out and particularly under condition of application of organic and inorganic forms of phosphorus.
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