SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 13 May 2009
Published in Soil Sci Soc Am J 73:1142-1149 (2009)
DOI: 10.2136/sssaj2008.0182
© 2009 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Pandey, C. B.
Right arrow Articles by Singh, R. K.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Pandey, C. B.
Right arrow Articles by Singh, R. K.
Agricola
Right arrow Articles by Pandey, C. B.
Right arrow Articles by Singh, R. K.
Related Collections
Right arrow Nitrogen

SOIL BIOLOGY & BIOCHEMISTRY

Soil Nitrogen Mineralization and Microbial Biomass Relation, and Nitrogen Conservation in Humid-Tropics

C. B. Pandeya,*, R. C. Srivastavaa and R. K. Singhb

a Central Agricultural Research Institute, Post Box 181, Port Blair-744101Andaman, India
b Resear. Centre of Central Soil and Water Conserv., Resear. and Training Institute, Kota, Rajasthan, India

* Corresponding author (cbpandey5{at}rediffmail.com).

The reciprocal relationship between microbial biomass C (MB-C) and net nitrification in the seasonally dry tropics can reduce nitrate (NO3) leaching losses, and be regarded as a mechanism of N conservation. The objective of the present study was to determine the influence of high seasonally prolonged rainfall on water-filled pore space (WFPS), net-nitrification rates (NNR), net-ammonification rates (NAR), pool sizes of NH4+–N and NO3–N, and MB-C in three major land-use systems (moist-evergreen, semi-evergreen forests, and home garden) in the equatorial humid tropical climate of South Andaman, India. Soil properties were examined to determine a mechanism of N conservation in the humid tropical soils. Across the land use systems, WFPS ranged from 68 to 84% during the wet season and 25 to 47% during wet season dry spells (48–72 h after wet season high rainfall). The rate of net-nitrification and NO3–N pool declined 10 to 17 times and 4 to 6 times, respectively during the high rainfall wet season in all the land use systems compared with wet season dry spells. On the contrary, ammonification rate and NH4+–N pool increased 7 to 34 times and 2 to 3 times, respectively during the wet season across land use systems compared with the wet season dry spell. Microbial biomass C was positively correlated with the NNR, but it was inversely correlated with the NH4+–N pool. The above observations suggest that NO3 N is likely reduced to NH4+ via a dissimilatory pathway during rainy periods (anaerobic conditions), which conserves N in the plant available form (NH4+) in the soils of the humid tropics.

Abbreviations: MB-C, microbial biomass carbon • NH4+–N, ammonium N pool • NAR, net ammonification rate • NMR, net mineralization rate • NNR, net nitrification rate • NO3–N, nitrate N pool • WFPS, water-filled pore space







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2009 by the Soil Science Society of America.