中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
N2O emission from a temperate forest soil during the freeze-thaw period: A mesocosm study

文献类型:期刊论文

作者Peng, Bo2,3; Sun, Jianfei2; Liu, Jun2; Dai, Weiwei2; Sun, Lifei2,3; Pei, Guangting2,3; Gao, Decai2,3; Wang, Chao2; Jiang, Ping2; Bai, Edith1,2
刊名SCIENCE OF THE TOTAL ENVIRONMENT
出版日期2019-01-15
卷号648页码:350-357
关键词N2O emission Freeze-thaw cycle Physical release Biological process Potential enzyme activities
ISSN号0048-9697
DOI10.1016/j.scitotenv.2018.08.155
英文摘要Nitrous oxide (N2O) is an important greenhouse gas and is involved in the destruction of ozone layer. However, the underlying mechanisms of the high soil N2O emission during the freeze-thaw (FT) period are still unclear. Here, we conducted a mesocosm study with high frequency in situ measurements to explore the responses of soil microbes to the FT cydes and their influences on soil N2O emission. We found the high N2O emission rate during the FT period was mainly due to the release of substrates, the maintenance of high enzyme activities at the freezing stage, and the fast recovery of microbial biomass nitrogen (MBN) and high microbial activities at the thawing stage. Physical isolation of previously produced N2O was an important mechanism for the higher N2O flux at the thawing stage. With increasing numbers of the FT cydes, MBN at the thawing stage remained stable and potential dehydrogenase activities at the thawing stage also remained stable after the first eight FT cydes and only declined during the last two cycles, suggesting the sustainability of the biological mechanisms. Our study suggests that although MBN declined, microbial enzymes could maintain high activities at a few degrees Celsius below zero in this temperate forest soil and produce high N2O fluxes even at the freezing stage, which were trapped under the ice layer and released at the thawing stage, resulting in high soil N2O emission during the FT period. (C) 2018 Elsevier B.V. All rights reserved.
资助项目Major State Basic Research Development Program of China (973 Program)[2014CB954400] ; Key Research Program of Frontier Sciences, CAS[QYZDB-SSWDQC006]
WOS研究方向Environmental Sciences & Ecology
语种英语
WOS记录号WOS:000447805500033
出版者ELSEVIER SCIENCE BV
源URL[http://210.72.129.5/handle/321005/123479]  
专题中国科学院沈阳应用生态研究所
通讯作者Bai, Edith
作者单位1.Northeast Normal Univ, Sch Geog Sci, Changchun 130024, Peoples R China
2.Chinese Acad Sci, Inst Appl Ecol, CAS Key Lab Forest Ecol & Management, Shenyang 110016, Liaoning, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Peng, Bo,Sun, Jianfei,Liu, Jun,et al. N2O emission from a temperate forest soil during the freeze-thaw period: A mesocosm study[J]. SCIENCE OF THE TOTAL ENVIRONMENT,2019,648:350-357.
APA Peng, Bo.,Sun, Jianfei.,Liu, Jun.,Dai, Weiwei.,Sun, Lifei.,...&Bai, Edith.(2019).N2O emission from a temperate forest soil during the freeze-thaw period: A mesocosm study.SCIENCE OF THE TOTAL ENVIRONMENT,648,350-357.
MLA Peng, Bo,et al."N2O emission from a temperate forest soil during the freeze-thaw period: A mesocosm study".SCIENCE OF THE TOTAL ENVIRONMENT 648(2019):350-357.

入库方式: OAI收割

来源:沈阳应用生态研究所

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