The effects of damming and dam regulation on a river-lake-aquifer system: 3D groundwater flow modeling of Poyang Lake (China)

被引:5
作者
Jiang, Wenyu [1 ]
Liu, Bo [1 ]
Li, Yunliang [2 ,3 ]
Lu, Chengpeng [1 ]
Shu, Longcang [1 ]
机构
[1] Hohai Univ, Coll Hydrol & Water Resources, 1 Xikang Rd, Nanjing 210098, Peoples R China
[2] Chinese Acad Sci, Nanjing Inst Geog & Limnol, 73 East Beijing Rd, Nanjing 210008, Peoples R China
[3] Poyang Lake Res Stn Wetland Ecosyst, 113 Jingang Rd, Jiujiang 332800, Peoples R China
基金
中国国家自然科学基金;
关键词
Poyang Lake; Lake-groundwater interaction; Groundwater flow simulation; Hydraulic dam; Regional groundwater storage; SURFACE-WATER; HYDROLOGIC EXCHANGE; CLIMATE-CHANGE; FLOODPLAIN; VEGETATION; DISCHARGE; DYNAMICS; RECHARGE; IMPACTS; BASIN;
D O I
10.1016/j.jhydrol.2024.131311
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Large numbers of dams are planned or constructed for hydroelectric power production, water supply, and flood control in many rivers around the world. While the social and environmental impacts of dams are now wellunderstood, there is little knowledge about the effects of dams on groundwater-surface water interactions in a complex lake -river-aquifer system. This study adopts a three-dimensional groundwater numerical model to quantify the potential impacts of dam construction, on regional groundwater flow system, exemplified by the proposed Poyang Lake Hydraulic Dam (PLHD) in China. Once implemented, the PLHD will regulate lake levels, artificially controlling the lake inundation area during the recession season (September-October) and the dry season (November -December). Modeling results indicated that the increase in lake infiltration induced by PLHD regulation would alter the regional water exchange pattern. The PLHD regulation will likely enhance the groundwater storage by 20.44 % in the general dry year (i.e., 2018), alleviating 78.1 % of the groundwater deficit in the extreme dry year (i.e., 2019). Additionally, the response of groundwater dynamics to the PLHD regulation exhibits significant spatial differences between the upstream and downstream areas of the dam, primarily depending on topographical changes. Overall, the PLHD regulation is most likely to impact groundwater levels across an area of approximately 5,700 km 2 , and the associated groundwater storage is anticipated to reach a stable state, under future long -term regulation. Our findings may guide policy -makers wishing to develop more suitable PLHD scheduling plans and floodplain protection strategies by providing reliable information regarding groundwater storage change and ecosystem succession.
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页数:14
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