Effects of a proposed hydraulic project on the surface water connectivity in Poyang Lake floodplain system, China: Numerical simulation and geostatistical analysis

被引:1
|
作者
Wang, Zixuan [1 ,2 ]
Xiao, Yang [1 ,2 ,3 ,4 ,5 ]
Zhang, Taotao [4 ]
Xu, Chen [6 ]
Gu, Ran [1 ,2 ]
Liu, Jiaming [1 ,2 ]
机构
[1] Hohai Univ, Natl Key Lab Water Disaster Prevent, Nanjing, Peoples R China
[2] Hohai Univ, Coll Water Conservancy & Hydropower Engn, Nanjing, Peoples R China
[3] Hohai Univ, Key Lab Hydrol Cycle, Hydrodynam Syst Minist Water Resources, Nanjing, Peoples R China
[4] Suzhou Univ Sci & Technol, Sch Environm Sci & Engn, Suzhou, Peoples R China
[5] Hohai Univ, Yangtze Inst Conservat & Dev, Nanjing, Peoples R China
[6] Suzhou Univ Sci & Technol, Sch Geog Sci & Geomatics Engn, Suzhou, Peoples R China
基金
中国国家自然科学基金;
关键词
Poyang Lake floodplain; Poyang Lake Hydraulic Project; Surface water connectivity; Hydrodynamic model; Geostatistical connectivity analysis; YANGTZE-RIVER FLOW; WETLAND CHANGES; IMPACT; DYNAMICS; DAM;
D O I
10.1016/j.ejrh.2023.101593
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Study Region: Poyang Lake, the largest freshwater lake in China, has been experiencing persistent shrinkage in recent years.Study Focus: The Poyang Lake Hydraulic Project (PLHP) was proposed to improve water resource and environment carrying capacity, its hydrological effects remain under investigation. This study combined a hydrodynamic model with geostatistical connectivity analysis, to quantify the influence of the PLHP on surface water connectivity in Poyang Lake.New Hydrological Insights for the Region: The PLHP enlarges inundated areas most in the recession period (September-November), accounting for 85% of the total increase throughout the operating period (September-March), and enhances the interconnection probability within these inundated regions. Statistical analysis reveals that the Connectivity Function (CF) in low connectivity conditions (CF <0.4) can be significantly increased by 0.1-0.9, primarily in areas with lower topographies. While for the saucer-shaped sub-lakes, the PLHP can rarely extend the connecting processes between the main lake and sub-lakes in low-water-level conditions below 13 m, which is the lowest threshold height of most sub-lakes. Moreover, most isolated sub-lakes have merged into the main lake when the water level is higher than 14 m, thus the PLHP is no longer effective in this condition. Therefore, the enhancement effect of the PLHP on the connectivity of sub-lakes is restricted in both high-and low-water-level years, and is most pronounced in the medium water-level year.
引用
收藏
页数:18
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