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土壤水分对土壤产生气态氮的厌氧微生物过程的影响
引用本文:李靳,康荣华,于浩明,王莹莹,姚萌,方运霆. 土壤水分对土壤产生气态氮的厌氧微生物过程的影响[J]. 应用生态学报, 2021, 32(6): 1989-1997. DOI: 10.13287/j.1001-9332.202106.010
作者姓名:李靳  康荣华  于浩明  王莹莹  姚萌  方运霆
作者单位:1.中国科学院沈阳应用生态研究所森林生态与管理重点实验室, 沈阳 110016;2.中国科学院大学, 北京 100049;3.辽宁省稳定同位素技术重点实验室, 沈阳 110016
基金项目:国家自然科学基金项目(41807320)资助
摘    要:气态氮[一氧化氮(NO)、氧化亚氮(N2O)和氮气(N2)]的释放是土壤氮损失的一种重要途径.硝化和反硝化作用是土壤气态氮损失的主要微生物过程,但是异养硝化作用、共反硝化作用和厌氧氨氧化过程对土壤气态氮损失的贡献尚不清楚.本研究利用15N标记和配对法,结合硝化抑制剂双氰胺(DCD),通过土壤培养试验来量化厌氧条件下各种...

关 键 词:15N标记法  15N配对法  一氧化氮  氧化亚氮  氮气  反硝化过程  异养硝化过程  共反硝化过程  土壤水分
收稿时间:2021-03-04

Effects of soil moisture on microbial processes of soil nitrogen gases production under anaerobic conditions
LI Jin,KANG Rong-hua,YU Hao-ming,WANG Ying-ying,YAO Meng,FANG Yun-ting. Effects of soil moisture on microbial processes of soil nitrogen gases production under anaerobic conditions[J]. The journal of applied ecology, 2021, 32(6): 1989-1997. DOI: 10.13287/j.1001-9332.202106.010
Authors:LI Jin  KANG Rong-hua  YU Hao-ming  WANG Ying-ying  YAO Meng  FANG Yun-ting
Affiliation:1.Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China;2.University of Chinese Academy of Sciences, Beijing 100049, China;3.Key Laboratory of Stable Isotope Techniques and Applications, Shenyang 110016, China
Abstract:Gaseous nitrogen (N) emission [nitric oxide (NO), nitrous oxide (N2O), and nitrogen (N2)] is an important pathway of soil N loss. Nitrification and denitrification are the main processes of gaseous N production in soil. However, the contribution of heterotrophic nitrification, co-denitrification, and anammox to gaseous N production remains uncertain. In a laboratory soil incubation experiment, we used the 15N labelling and pairing technique, combining the nitrification inhibitor dicyandiamide (DCD), to quantify the contribution of different microbial processes to soil NO, N2O and N2 production under anaerobic conditions. The results showed that after 24 h anaerobic incubation, the highest total 15N recovery of three gases occurred at 65% water filled pore space (WFPS), accounting for 20.0% of total added 15N. Denitrification contributed 49.9%-94.1%, 29.0%-84.7%, and 58.2%-85.8% to the production of NO, N2O and N2 respectively, suggesting that denitrification was the predominant process of those three N gases emission. Heterotrophic nitrification was an important pathway of NO and N2O production, particularly at conditions with low soil water content (10% WFPS), with its contribution to those two N gases production being 50.1% and 42.8%, respectively. Co-denitrification contributed 10.6%-30.7% of N2O production. For N2 production, the total contribution of co-denitrification and anammox was 14.2%-41.8%. The role of co-denitrification can not be ignored for N2O and N2 production. Our results demonstrated that the 15N labelling and pairing technique is a promising tool to quantify the contribution of different microbial processes to gaseous N loss.
Keywords:15N labelling  15N pairing technique  NO  N2O  N2  denitrification  heterotrophic nitrification  co-denitrification  soil moisture  
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