Anaerobic ammonium oxidation and denitrification in a paddy soil as affected by temperature, pH, organic carbon, and substrates
Anaerobic ammonium oxidation and denitrification in a paddy soil as affected by temperature, pH, organic carbon, and substrates
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DOI:
10.1007/s00374-018-1263-z
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发表时间:
2018-01
影响因子:
6.5
通讯作者:
J. Shan;Pinpin Yang;X. Shang;M. M. Rahman-M.;M. M. Rahman-M.;Xiaoyuan Yan
中科院分区:
文献类型:
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作者:
J. Shan;Pinpin Yang;X. Shang;M. M. Rahman-M.;M. M. Rahman-M.;Xiaoyuan Yan
Anaerobic ammonium oxidation (anammox process) widely occurs in paddy soil and may substantially contribute to permanent N removal; however, little is known about the factors controlling this process. Here, effects of temperature, pH, organic C, and substrates on potential rate of anammox and the relative contribution of anammox to total N2production in a paddy soil were investigated via slurry incubation combined with15N tracer technique. Anammox occurred over a temperature range from 5 to 35 °C with an optimum rate at 25 °C (1.7 nmol N g−1h−1) and a pH range from 4.8 to 10.1 with an optimum rate at pH 7.3 (1.7 nmol N g−1h−1). The presence of glucose and acetate (5–100 mg C L−1) significantly inhibited anammox activities and the ratio of anammox to total N2production. The response of potential rates of anammox to ammonium concentrations fitted well with Michaelis-Menten relationship showing a maximum rate (Vmax) of 4.4 nmol N g−1h−1and an affinity constant (Km) of 6.3 mg NH4+-N L−1. Whereas, nitrate addition (5–15 mg15NO3−-N L−1) significantly inhibited anammox activities and the ratio of anammox to total N2production. Our results provide useful information on factors controlling anammox process and its contribution to N loss in the paddy soil.