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Published in Soil Sci Soc Am J 50:308-313 (1986)
© 1986 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Distribution of Nitrogen Forms and Availability Indices in Profiles of Differently Managed Soil Types1

Aviva Hadas, Sala Feigenbaum, A. Feigin and Rita Portnoy2

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.


NOTES

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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