中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Terrigenous organic carbon drives methane dynamics in cascade reservoirs in the upper Yangtze China

文献类型:期刊论文

作者Zhang, Yuanyuan1,2; Su, Youheng2,3; Li, Zhe1,2; Guo, Shuhui4; Lu, Lunhui1,2; Zhang, Bin2; Qin, Yu3
刊名WATER RESEARCH
出版日期2022-07-01
卷号219页码:12
关键词Methane dynamics Terrigenous POC Carbon footprint Cascade reservoirs Hydropower production
ISSN号0043-1354
DOI10.1016/j.watres.2022.118546
通讯作者Li, Zhe(lizhe@cigit.ac.cn)
英文摘要Methane (CH4) emissions from freshwaters to the atmosphere have a profound impact on global atmospheric greenhouse gas (GHG) concentrations. Anthropogenic footprints such as dam construction and reservoir operation significantly changed the fate and transport of CH4 in freshwaters. The source of particulate organic carbon (POC) in reservoirs is a critical factor controlling CH4 production and emissions. However, little is known of how reservoir operation mediates the transport of POC and regulates CH4 accumulation in cascade hydroelectric reservoirs. Here, spatial and temporal variations in POC and CH4 were explored in the Xiluodu (XLD) and Xiangjiaba (XJB) reservoirs which are deep valley cascade reservoirs located in the main channel of the upper Yangtze River. Based on the delta 13C-POC and N/C mole ratio of particulate organic matter, the results of multiendmember stable isotope mixing models by a Bayesian model showed that terrigenous POC and autochthonous POC accounted for approximately 55% +/- 18% and 43% +/- 19% (SD, n = 179) of POC, respectively. Together with other hydrological and environmental parameters, we found that the input of terrigenous POC was dominantly influenced by water level variations and flow regulation due to reservoir operation. The cumulative effect of POC caused by cascade dams was not apparent. Terrigenous POC were more likely to drive CH4 accumulation in our study. Evident low level of CH4 in both reservoirs were likely affected by low sedimentation of POC and microbial CH4 oxidation. We hope our study could provide a conceptual framework for further modeling of CH4 dynamics in cascade reservoirs.
资助项目National Natural Science Foundation of China[51861125204] ; National Natural Science Foundation of China[51679226] ; National Natural Science Foundation of China[42107273] ; Chinese Academy of Sciences[cstc2020jcyj- jqX0010] ; Chongqing Natural Science Funds for Distinguished Young Scientists ; China Three Gorges Corporation
WOS研究方向Engineering ; Environmental Sciences & Ecology ; Water Resources
语种英语
WOS记录号WOS:000803703800005
出版者PERGAMON-ELSEVIER SCIENCE LTD
源URL[http://119.78.100.138/handle/2HOD01W0/15949]  
专题中国科学院重庆绿色智能技术研究院
通讯作者Li, Zhe
作者单位1.Univ Chinese Acad Sci, Coll Resources & Environm, Chongqing Sch, Chongqing 400714, Peoples R China
2.Chinese Acad Sci, Chongqing Inst Green & Intelligent Technol, CAS Key Lab Reservoir Environm, Chongqing 400714, Peoples R China
3.Chongqing Jiaotong Univ, Coll River & Ocean Engn, Chongqing 400074, Peoples R China
4.Minist Ecol & Environm Peoples Republ China, Foreign Environm Cooperat Ctr, Beijing 100035, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Yuanyuan,Su, Youheng,Li, Zhe,et al. Terrigenous organic carbon drives methane dynamics in cascade reservoirs in the upper Yangtze China[J]. WATER RESEARCH,2022,219:12.
APA Zhang, Yuanyuan.,Su, Youheng.,Li, Zhe.,Guo, Shuhui.,Lu, Lunhui.,...&Qin, Yu.(2022).Terrigenous organic carbon drives methane dynamics in cascade reservoirs in the upper Yangtze China.WATER RESEARCH,219,12.
MLA Zhang, Yuanyuan,et al."Terrigenous organic carbon drives methane dynamics in cascade reservoirs in the upper Yangtze China".WATER RESEARCH 219(2022):12.

入库方式: OAI收割

来源:重庆绿色智能技术研究院

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