4.7 Article

Dissimilatory nitrate/nitrite reduction to ammonium (DNRA) pathway dominates nitrate reduction processes in rhizosphere and non-rhizosphere of four fertilized farmland soil

期刊

ENVIRONMENTAL RESEARCH
卷 186, 期 -, 页码 -

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.envres.2020.109612

关键词

DNRA; Denitrification; Anammox; DAMO; Arid farmland soil; N cycle

资金

  1. National Natural Science Foundation of China [41671471, 41322012, 91851204]
  2. Local Innovative and Research Teams Project of Guangdong Pearl River Talents Program [2017BT01Z176]
  3. Project of National Joint Research Center for Yangtze River Conservation [2019-LHYJ-01-0103]
  4. Yangtze River Protection Project of Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences [RCEES-CJBH-2019-03]
  5. Key Research Program of Frontier Sciences, Chinese Academy of Sciences [QYZDJ-SSW-DQC013]
  6. Excellent Innovation Project of Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences [RCEES-EEI-2019-02]
  7. State Key Joint Laboratory of Environment Simulation and Pollution Control (Research Center for Eco-environmental Sciences, Chinese Academy of Sciences) [18Z02ESPCR]

向作者/读者索取更多资源

Nitrate (NO3-) reduction partitioning between denitrification, anaerobic ammonium oxidation (anammox), denitrifying anaerobic methane oxidation (DAMO), and dissimilatory nitrate reduction to ammonium (DNRA), can influence the nitrogen (N) use efficiency and crop production in arid farmland. The microbial structure, function and potential rates of denitrification, anammox, DAMO and DNRA, and their respective contributions to total NO3- reduction were investigated in rhizosphere and non-rhizosphere soil of four typical crops in north China by functional gene amplification, high-throughput sequencing, network analysis and isotopic tracing technique. The measured denitrification and DNRA rate varied from 0.0294 to 20.769 nmol N g(-1) h(-1) nd 2.4125-58.682 nmol N g(-1) h(-1), respectively, based on which DNRA pathway contributed to 84.44 +/- 14.40% of dissimilatory NO3- reduction, hence dominated NO3- reduction processes compared to denitrification. Anammox and DAMO were not detected. High-throughput sequencing analysis on DNRA nrfA gene, and denitrification nirS and nirK genes demonstrated that these two processes did not correlate to corresponding gene abundance or dominant genus. RDA and Pearson's correlation analysis illustrated that DNRA rate was significantly correlated with the abundance of Chthiniobacter, as well as total organic matter (TOM); denitrification rate was significantly correlated with the abundance of Lautropia, so did TOM. Network analysis showed that the genus performed DNRA was the key connector in the microbial community of dissimilatory nitrate reducers. This study simultaneously investigated the dissimilatory nitrate reduction processes in rhizosphere and non-rhizosphere soils in arid farmland, highlighting that DNRA dominated NO3- reduction processes against denitrification. As denitrification results in N loss, whereas DNRA contributes to N retention, the relative contributions of DNRA versus denitrification activities should be considered appropriately when assessing N transformation processes and N fertilizer management in arid farmland fields.

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