文献类型：期刊文献

英文题名：Inter-Annual Variations of Methane Emission from an Open Fen on the Qinghai-Tibetan Plateau: A Three-Year Study

作者：Chen, Huai[1,2] Wu, Ning[1] Wang, Yanfen[3] Zhu, Dan[1] Zhu, Qiu'an[2] Yang, Gang[2] Gao, Yongheng[4] Fang, Xiuqin[5] Wang, Xu[6] Peng, Changhui[2,5]

第一作者：Chen, Huai

通信作者：Chen, H[1]

机构：[1]Chinese Acad Sci, Chengdu Inst Biol, Chengdu, Peoples R China;[2]NW A&F Univ, Lab Ecol Forecasting & Global Change, Coll Forestry, Yangling, Peoples R China;[3]Univ Chinese Acad Sci, Beijing, Peoples R China;[4]Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu, Peoples R China;[5]Univ Quebec Montreal, Inst Environm Sci, Montreal, PQ, Canada;[6]Chinese Acad Forestry, Res Inst Trop Forestry, Guangzhou, Guangdong, Peoples R China

年份：2013

卷号：8

期号：1

外文期刊名：PLOS ONE

收录：;Scopus(收录号：2-s2.0-84872352904);WOS:【SCI-EXPANDED(收录号:WOS:000314759400093)】；

基金：This study was supported by the National Natural Science Foundation of China (No. 31100348), Natural Science Foundation Project of CQ CSTC (2009BB7182), Natural Sciences and Engineering Research Council of Canada (NSERC) discovery grant, and the China QianRen programme. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

语种：英文

摘要：The study aimed to understand the inter-annual variations of methane (CH4) emissions from an open fen on the Qinghai-Tibetan Plateau (QTP) from 2005 to 2007. The weighted mean CH4 emission rate was 8.37 +/- 11.32 mg CH4 m(-2) h(-1) during the summers from 2005 to 2007, falling in the range of CH4 fluxes reported by other studies, with significant inter-annual and spatial variations. The CH4 emissions of the year of 2006 (2.11 +/- 3.48 mg CH4 m(-2) h(-1)) were 82% lower than the mean value of the years 2005 and 2007 (13.91 +/- 17.80 mg CH4 m(-2) h(-1) and 9.44 +/- 14.32 mg CH4 m(-2) h(-1), respectively), responding to the inter-annual changes of standing water depths during the growing season of the three years. Significant drawdown of standing water depth is believed to cause such significant reduction in CH4 emissions from wetlands in the year 2006, probably through changing the methanogen composition and decreasing its community size as well as activating methanotrophs to enhance CH4 oxidation. Our results are helpful to understand the inter-annual variations of CH4 emission and provide a more reasonable regional budget of CH4 emission from wetlands on the QTP and even for world-wide natural wetlands under climate change.