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ABSTRACT
Various chemical methods have been used to predict the N mineralization potential of soils, but studies have been restricted mainly to surface soil layers, to which most N mineralization is attributed. In this study, the distribution of N forms, extracted from soil by different chemical methods, and the relationship between them were determined within the profiles of several soil types. All N parameters tested were significantly correlated with total N. The fractions of several N parameters of total N changed with soil depth: oxidative release of NH4+ by acid KMnO4, N extracted by NaHCO3, and NH4+ and hexosamine in soil acid hydrolyzate all increased, whereas amino acids and amidase activity decreased with soil depth. Soil type also influenced some N parameters: acid KMnO4 extracted relatively more NH4+ from calcareous than noncalcareous soils; a smaller fraction of total N was acid hydrolyzable in soils with a greater surface area; and amidase activity was considerably higher in cultivated clay soils.
1 Contribution from the ARO, The Volcani Center, Bet Dagan, Israel, no. 1423-E, 1985 Series. This research was supported by a grant from the U.S.-Israel (Binational) Agricultural Research and Development Fund (BARD).
2 Soil Scientists and Chemist, respectively, Dep. of Soil Chemistry and Plant Nutrition, ARO, P.O. Box 6, Bet Dagan, Israel.
Received for publication June 6, 1985.
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