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Long-term application of lime or pig manure rather than plant residues suppressed diazotroph abundance and diversity and altered community structure in an acidic Ultisol
Biological fixation of atmospheric dinitrogen (N2) is an important process that replenishes biologically available nitrogen (N) in soil and helps minimize the use of inorganic N fertilizer in agricultural ecosystems. Diazotrophs are key fixers of atmospheric N2 in a range of soil types, however, the...
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Published in: | Soil biology & biochemistry 2018-08, Vol.123, p.218-228 |
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Main Authors: | , , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Biological fixation of atmospheric dinitrogen (N2) is an important process that replenishes biologically available nitrogen (N) in soil and helps minimize the use of inorganic N fertilizer in agricultural ecosystems. Diazotrophs are key fixers of atmospheric N2 in a range of soil types, however, there is uncertainty about how they respond to long-term fertilization. Here, using the nifH gene as a molecular marker, we investigated the long-term effects of inorganic and organic fertilization on diazotroph abundance and community structure in an acidic Ultisol. The field experiment ran for 27 years and comprised seven treatments: no fertilization (control); inorganic NPK fertilizer (N); inorganic NPK fertilizer + lime (CaCO3) (NL); inorganic NPK fertilizer + peanut straw (NPS); inorganic NPK fertilizer + rice straw (NRS); inorganic NPK fertilizer + radish (NR); and inorganic NPK fertilizer + pig manure (NPM). Long-term application of fertilizer reduced the abundance and diversity of nifH gene compared with the control (P |
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ISSN: | 0038-0717 1879-3428 |
DOI: | 10.1016/j.soilbio.2018.05.018 |