Evaluation of ecological instream flow considering hydrological alterations in the Yellow River basin, China

被引:76
|
作者
Zhang, Qiang [1 ,2 ,3 ,4 ]
Zhang, Zongjiao [5 ]
Shi, Peijun [1 ,2 ,3 ,4 ]
Singh, Vijay P. [6 ,7 ]
Gu, Xihui [8 ]
机构
[1] Beijing Normal Univ, Key Lab Environm Changes & Nat Hazards, Beijing 100875, Peoples R China
[2] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China
[3] Beijing Normal Univ, Fac Geog Sci, Beijing 100875, Peoples R China
[4] Beijing Normal Univ, Acad Disaster Reduct & Emergency Management, Beijing 100875, Peoples R China
[5] Sun Yat Sen Univ, Dept Water Resources & Environm, Guangzhou 510275, Guangdong, Peoples R China
[6] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX USA
[7] Texas A&M Univ, Zachry Dept Civil Engn, College Stn, TX USA
[8] China Univ Geosci, Sch Environm Studies, Wuhan 430074, Hubei, Peoples R China
基金
美国国家科学基金会; 中国国家自然科学基金;
关键词
Ecological instream flow; Indicator of Hydrological Alteration (IHA); Biodiversity; Ecodeficit; Ecosurplus; Hydrological alterations; Yellow River basin; SEMIARID REGIONS; WATER; MIDDLE; REQUIREMENTS; REACH; DAMS;
D O I
10.1016/j.gloplacha.2017.11.012
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The Yellow River is the second largest river in China and is the important source for water supply in the northwestern and northern China. It is often regarded as the mother river of China. Owing to climatic change and intensifying human activities, such as increasing withdrawal of water for meeting growing agricultural irrigation needs since 1986, the flow of Yellow River has decreased, with serious impacts on the ecological environment. Using multiple hydrological indicators and Flow Duration Curve (DFC)-based ecodeficit and ecosurplus, this study investigates the impact of hydrological alterations, such as the impact of water reservoirs or dams, on downstream ecological instream flow. Results indicate that: (1) due to the impoundment and hydrological regulations of water reservoirs, occurrence rates and magnitudes of high flow regimes have decreased and the decrease is also found in the magnitudes of low flow events. These changes tend to be more evident from the upper to the lower Yellow River basin; (2) human activities tend to enhance the instream flow variability, particularly after the 1980s;(3) the ecological environment in different parts of the Yellow River basin is under different degrees of ecological risk. In general, lower to higher ecological risk can be detected due to hydrological alterations from the upper to the lower Yellow River basin. This shows that conservation of ecological environment and river health is facing a serious challenge in the lower Yellow River basin; (4) ecological in stream flow indices, such as ecodeficit and ecosurplus, and IHA32 hydrological indicators are in strong relationships, suggesting that ecodeficit and ecosurplus can be regarded as appropriate ecological indicators for developing measures for mitigating the adverse impact of human activities on the conservation of ecological environment in the Yellow River basin.
引用
收藏
页码:61 / 74
页数:14
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