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大型水库运行对坝下游河段水位和流量的影响:以三峡水库为例

Influence of Large Reservoir Operation on Water-Levels and Flows in Reaches below Dam: Case Study of the Three Gorges Reservoir.

作者信息

Yang Yunping, Zhang Mingjin, Zhu Lingling, Liu Wanli, Han Jianqiao, Yang Yanhua

机构信息

Key Laboratory of Engineering Sediment, Tianjin Research Institute for Water Transport Engineering, Ministry of Transport, Tianjin, 300456, China.

State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, 430072, China.

出版信息

Sci Rep. 2017 Nov 15;7(1):15640. doi: 10.1038/s41598-017-15677-y.

Abstract

The Three Gorges Project (TGP) is the world's largest water conservation project. The post-construction low-flow water level at the same discharge below the dam has declined, but there remains disagreement over whether the flood level has increased. Measured water levels and upstream and downstream flow data from 1955 to 2016 show that, post-construction: (1) the low-flow water level at the same discharge decreased, and the lowest water level increased due to dry-season reservoir discharge; (2) the decline of the low-flow water level below the dam was less than the undercutting value of the flow channel of the river; (3) the flood level at the same discharge below the dam was slightly elevated, although peak water levels decreased; (4) flood characteristics changed from a high discharge-high flood level to a medium discharge - high flood level; and (5) an expected decline in the flood level downstream was not observed. Channel erosion and the adjustment of rivers and lakes tend to reduce flood levels, while river bed coarsening, vegetation, and human activities downstream increase the flood level. Although the flood control benefits of the Three Gorges Dam (TGD) and the upstream reservoirs are obvious, increased elevation of the downstream flood level remains a concern.

摘要

三峡工程是世界上最大的水利枢纽工程。大坝建成后,相同流量下坝址下游枯水期水位有所下降,但对于汛期水位是否上升仍存在争议。1955年至2016年实测水位及上下游流量资料表明,大坝建成后:(1)相同流量下枯水期水位下降,因枯水期水库泄流,最低水位有所上升;(2)坝址下游枯水期水位下降幅度小于河道下切值;(3)相同流量下坝址下游汛期水位略有抬高,尽管洪峰水位有所降低;(4)洪水特性从高流量-高水位型转变为中流量-高水位型;(5)未观测到下游预期的水位下降。河道冲刷以及河湖调整往往会降低水位,而河床粗化、植被及下游人类活动则会抬高水位。尽管三峡大坝及上游水库的防洪效益显著,但下游水位的升高仍令人担忧。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a59/5688129/240fa8a1555c/41598_2017_15677_Fig4_HTML.jpg

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