Open AccessSurface methane emissions from different land use types during various water levels in three major drawdown areas of the Three Gorges Reservoir
Author(s) -
Yang Le,
Lu Fei,
Wang Xiaoke,
Duan Xiaonan,
Song Wenzhi,
Sun Binfeng,
Chen Shuai,
Zhang Qianqian,
Hou Peiqiang,
Zheng Feixiang,
Zhang Ye,
Zhou Xiaoping,
Zhou Yongjuan,
Ouyang Zhiyun
Publication year - 2012
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2011jd017362
Subject(s) - three gorges , drawdown (hydrology) , sink (geography) , environmental science , hydrology (agriculture) , methane emissions , paddy field , methane , water level , groundwater , geology , aquifer , agronomy , ecology , geography , geotechnical engineering , cartography , biology
Methane (CH 4 ) emissions from the drawdown area of the Three Gorges Reservoir (TGR) have not been thoroughly investigated even though the drawdown area encompasses one third of the reservoir surface. In this study, CH 4 emissions from different land uses were measured in the TGR drawdown area. The average diffusive CH 4 emissions were 2.61, 0.19, 0.18, and 0.12 mg CH 4 m −2 h −1 in rice paddies, fallow lands, deforested lands, and croplands, respectively, and were positively related to the duration of the inundated season among the latter three land uses. On average the drawdown areas studied here (except rice paddies) were sources in the inundated season (0.22 ± 0.26 mg CH 4 m −2 h −1 ) and a sink in the drained season (−0.008 ± 0.035 mg CH 4 m −2 h −1 ). The water level was the dominant factor that controlled whether the drawdown area was either inundated or drained, which in turn determined whether the drawdown area was a source or sink of CH 4 emissions. The average diffusive CH 4 emissions from the fallow lands, croplands, and deforested lands increased as the distance from the dam increased from Zigui (0.10 ± 0.15 mg CH 4 m −2 h −1 ) to Wushan (0.15 ± 0.29 mg CH 4 m −2 h −1 ) to Yunyang (0.24 ± 0.27 mg CH 4 m −2 h −1 ), which could reflect different sediment characteristics and water velocities. The total CH 4 emission from the drawdown area was estimated to range from 1033.5 to 1333.9 Mg CH 4 yr −1 , which would account for 42–54% of the total CH 4 emissions from the water surface of TGR.