Effects of carbon input on soil carbon stability and nitrogen dynamics
•Soil carbon stability and nitrogen dynamics in long-term experiment was analyzed.•Application of FYM in addition to NPK produced greater size of resistant C pool.•Additional carbon input in NPK plot had no effect on resistant carbon pool.•Carbon stability significantly affected the N dynamics in so...
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Published in | Agriculture, ecosystems & environment Vol. 189; pp. 36 - 42 |
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Main Authors | , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Oxford
Elsevier B.V
01.05.2014
Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | •Soil carbon stability and nitrogen dynamics in long-term experiment was analyzed.•Application of FYM in addition to NPK produced greater size of resistant C pool.•Additional carbon input in NPK plot had no effect on resistant carbon pool.•Carbon stability significantly affected the N dynamics in soil.•N availability in soil is linearly related with acid-hydrolyzable C pool.
Improved understanding of the process of carbon (C) stabilization is critical to managing emissions from agricultural soils and optimizing crop yield. We assessed soil organic C (SOC) stability and nitrogen (N) dynamics in a long-term fertilization experiment (started in 1972) conducted at three different locations in India (Jabalpur-Vertisol, Palampur-Alfisol and Ranchi-Alfisol). We measured soil organic C (SOC), C pools and stocks in the treatments of no fertilization as control, inorganic fertilization as NPK and integrated fertilization as NPK+farm yard manure (FYM). Quantification of different SOC pools was done by a procedure of acid hydrolysis followed by a long-term (247 days) incubation study. Based on crop yield and C storage, NPK+FYM was the best treatment for improving crop productivity and SOC sequestration. Integrated fertilization for 38 years increased SOC across sites. In the NPK treatment, additional C input (3–9 times higher) in the form of root biomass did not significantly change C pools. Application of FYM in addition to NPK enhanced the acid non-hydrolysable fraction of SOC across sites. Stability of SOC significantly influenced N dynamics in soil and the availability of N in soil is correlated with the amount of C in the acid-hydrolysable pool (R2=0.64, p=0.01) but not with SOC (R2=0.12, p=0.01). Long-term use of chemical fertilizers did not significantly affect soil total N content. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0167-8809 1873-2305 |
DOI: | 10.1016/j.agee.2014.03.019 |