Artificial tide generation and its effects on the water environment in the backwater of Three Gorges Reservoir

被引:33
|
作者
Sha, Yukun [1 ,2 ,4 ]
Wei, Yongping [3 ]
Li, Weipeng [1 ,2 ]
Fan, Jihui [1 ,2 ]
Cheng, Genwei [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Mt Hazard & Environm, Chengdu 610041, Peoples R China
[2] Chinese Acad Sci, Key Lab Mt Surface Proc & Ecol Regulat, Chengdu 610041, Peoples R China
[3] Univ Melbourne, Australian China Ctr Water Resources Res, Parkville, Vic 3010, Australia
[4] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
关键词
Three Gorges Reservoir; Water bloom control; Hydropower daily operation; Artificial tide generation; YANGTZE-RIVER; ESTUARY; CYCLE; EUTROPHICATION; CHINA; BAY; DISPERSION; NUTRIENTS; SEDIMENT; DYNAMICS;
D O I
10.1016/j.jhydrol.2015.06.020
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Since the water impounding of the Three Gorges Reservoir (TGR) in 2003, the water stage in the backwater region increased from 65 m before water impounding to 145 m, and the velocity of the stream flow decreased significantly. The outflows of the tributaries that flow into TGR were also obstructed by the backwater. Stopping the stream flow prevented the pollutants from diffusing and transporting themselves into the water body, hence polluting the water in several tributaries. The authors proposed an artificial tide generation approach to solve this problem. The man-made flood peak in the downstream and the waves of the water stage in the upstream of the TGR can be produced by operating hydropower generators daily to deal with peak-and-bottom variations in the electricity demand. These waves will propagate upwards and form artificial tides in the backwater area. The water stage variation will intensify the flow exchange between the main stem and the tributaries as well as enhance the diffusion of pollutants, which will subsequently decrease the eutrophication of the water body in the outlet of branches as well as relieve the algal bloom problem in the region. The daily operations in the reservoir were simulated and tested by using the proposed hydrodynamic model of TGR. The hydropower operation for the peak load of electricity demand will produce artificial tides in the backwater area of TGR as well as increase the water stage variation from 0.30 m to 0.50 m within a day. This periodic fluctuation of water stage waves will intensify the water exchange between the main reach of Changjiang (Yangtze River) and its tributaries with an additional inflow or outflow of up to 300-500 m(3)/s, which is equivalent to the average discharge of these tributaries during the summer. The artificial tide generation can enhance the internal exchange of backwater as well as improve the water environment condition in the backwater area. This operation approach provides a new technology for controlling the water quality in reservoirs as well as enhances environmental protection and resource utility. Crown Copyright (C) 2015 Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:230 / 237
页数:8
相关论文
共 50 条
  • [41] Contribution of heterotrophic bacterioplankton to cyanobacterial bloom formation in a tributary backwater area of the Three Gorges Reservoir, China
    Lunhui Lu
    Linlin Xu
    Jixiang Yang
    Zhe Li
    Jinsong Guo
    Yan Xiao
    Juanjuan Yao
    Environmental Science and Pollution Research, 2018, 25 : 27402 - 27412
  • [42] Total phosphorus model in Lake Gaoyang during the period of high water level in Pengxi River backwater zone, Three Gorges Reservoir
    He B.
    Li Z.
    Feng J.
    Xiao Y.
    Guo J.
    Li, Zhe (Lizhe@cigit.ac.cn), 1600, Science Press (28): : 295 - 302
  • [43] Water temperature exhibits an overwhelming effect on the spatial allocation of sediment phosphorus fractions in the permanent backwater area of the Three Gorges Reservoir, China
    Zhang, Daoxi
    Zhang, Zhiyong
    Muller, Jan-Peter
    Zhu, Liming
    Zhang, Sanfeng
    Wan, Ji
    Shi, Fang
    Xi, Zou
    Shi, Yulong
    WATER RESEARCH, 2025, 276
  • [44] Study on sediment problem in Chongqing primary city zone in fluctuating backwater reach of Three Gorges Reservoir
    Cheng, CG
    Luan, C
    PROCEEDINGS OF THE NINTH INTERNATIONAL SYMPOSIUM ON RIVER SEDIMENTATION, VOLS 1-4, 2004, : 876 - 880
  • [45] Investigation of phytoplankton and assessment of algal diversity on backwater area of Xiaojiang river in Three Gorges reservoir after its initiate impounding to the water level of 156 m in spring
    Key Laboratory of Three Gorges Reservoir Region's Eco-Environment, Faculty of Urban Construction and Environmental Engineering, Chongqing University, Chongqing 400045, China
    Huanjing Kexue, 2008, 10 (2710-2715):
  • [46] Spatial variation of soil phosphorus in the water level fluctuation zone of the Three Gorges Reservoir: Coupling effects of elevation and artificial restoration
    Qin, Dongming
    Li, Shanze
    Wang, Jingfu
    Wang, Dengjun
    Liao, Peng
    Wang, Yuchun
    Zhu, Zhiqiang
    Dai, Zhihui
    Jin, Zuxue
    Hu, Xinping
    Qiu, Shuoru
    Ma, Yiming
    Chen, Jingan
    SCIENCE OF THE TOTAL ENVIRONMENT, 2023, 905
  • [47] Simulation of Reservoir Sediment Flushing of the Three Gorges Reservoir Using an Artificial Neural Network
    Li, Xueying
    Qiu, Jun
    Shang, Qianqian
    Li, Fangfang
    APPLIED SCIENCES-BASEL, 2016, 6 (05):
  • [48] Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries
    Long, Liang-Hong
    Xu, Hui
    Ji, Dao-Bin
    Cui, Yu-Jie
    Liu, De-Fu
    Song, Lin-Xu
    ENVIRONMENTAL EARTH SCIENCES, 2016, 75 (22)
  • [49] EFFECTS OF ARTIFICIAL FLOODING ON WATER QUALITY OF A FLOODPLAIN BACKWATER
    Lizotte, R. E., Jr.
    Shields, F. D., Jr.
    Knight, S. S.
    Cooper, C. M.
    Testa, S., III
    Bryant, C. T.
    RIVER RESEARCH AND APPLICATIONS, 2012, 28 (10) : 1644 - 1657
  • [50] Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries
    Liang-Hong Long
    Hui Xu
    Dao-Bin Ji
    Yu-Jie Cui
    De-Fu Liu
    Lin-Xu Song
    Environmental Earth Sciences, 2016, 75