长江科学院院报

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梯级电站调峰驱动的河道洪水波传播特征分析

白治朋1(), 黄建平2, 刘新健3, 刘新波1, 文勇波1, 赵新益1, 栾华龙4, 杨忠勇5()   

  1. 1.中国长江电力股份有限公司,武汉 430014
    2.重庆渝方建筑工程设计有限公司,重庆 400020
    3.重庆市建筑科学研究院有限公司,重庆 400042
    4.长江科学院河流研究所,武汉 430019
    5.三峡大学 水利与环境学院,湖北 宜昌 443002
  • 收稿日期:2023-10-19 修回日期:2024-05-25 出版日期:2024-06-11
  • 通信作者: 杨忠勇(1984 — ),男,重庆忠县人,副教授,博士,研究方向为梯级水库优化调度。 Email: ayong0710@163.com
  • 作者简介:白治朋(1992 — ),男,陕西榆林人,高级工程师,硕士,研究方向为水库大坝防洪安全。Email: bai_zhipeng@ctg.com.cn
  • 基金资助:
    湖北省自然科学基金(2022CFB207);重庆市住房和城乡建设委员会科技项目(城科字2023第6-14号);湖北省高校优秀中青年科技创新团队(T2021003);长江科学院开放研究基金(CKWV20221003/KY);国家自然科学基金(42006156)

Analysis of flood propagation driven in the river between two dams by hydropeaking regulation in cascade reservoirs

BAI Zhi-peng1(), HUANG Jian-ping2, LIU Xin-Jian3, LIU Xin-bo1, WEN Yong-bo1, ZHAO Xin-yi1, LUAN Hua-long4, YANG Zhong-yong5()   

  1. 1. China Yangtze Power Co., Ltd., Wuhan 430014, China
    2. Chongqing Yufang Construction Engineering Design Co., Ltd., Chongqing 400020, China
    3. Chongqing Construction Science Research Institute Co. Ltd., Chongqing 400042, China
    4. River Department, Changjiang River Scienti?c Research Institute, Wuhan 430010, China
    5. College of Hydraulic and Environmental Engineering, China Three Gorges University, Yichang 443002, China
  • Received:2023-10-19 Revised:2024-05-25 Published:2024-06-11

摘要:

基于2018年实测水位、流量数据和一维解析模型,论文中重点讨论了梯级电站调峰驱动的洪水波在两坝间河道的传播过程。在三峡和葛洲坝同时进行日调峰的背景下,两个电站的出库流量均呈显著的日波动和半日波动现象,两电站的流量日波动幅度平均分别约在1500~2000 m3/s和1200~1500 m3/s之间,黄陵庙和南津关两个水位站的水位日波动幅度均在0.5~0.8m之间。基于一维解析模型能够很好的模拟和再现两坝间河道的水位和流量波动过程。模型模拟结果分析表明,两坝间河道洪水波以周期为1.2 h的高频驻波进行传播,驻波的最大水位和流量振幅分别约为2.1 cm和210 m3/s。该洪水波是由两个电站调峰流量共同驱动和叠加生成的,下游葛洲坝电站调峰时间对河道洪水波有显著影响,若将调峰时间由现行的0.6 h调整到1.2 h,洪水波振幅将显著增强。河道底摩擦系数对洪水波生成时的波高影响较小,但会影响洪水波在传播过程中的衰减速度。

关键词: 电站调峰, 洪水波, 解析模型, 驻波, 波能衰减

Abstract:

Based on the measured data of water level and discharge in 2018 and one-dimensional analytical model, this paper focuses on the propagation process of flood wave in the river between two dams driven by hydropeaking regulation. During daily hydropeaking regulation of Three Gorges dam and Gezhouba dam, the outflow flow of both two dams shows significant daily and semi-daily fluctuation, the average daily fluctuation range of the two power stations is about 1500-2000 m3/s and 1200-1500 m3/s, respectively. The daily fluctuation of water level in Huanglingmiao and Nanjinguan stations is about 0.5-0.8m. Based on one-dimensional analytical model, the fluctuation process of water level and discharge between two dams can be simulated and reproduced well. The simulation results show that the flood waves in the river between two dams are propagated by high frequency standing waves with a period of 1.2h, and the maximum water level and flow amplitude of standing waves are about 2.1 cm and 210 m3/s, respectively. The flood wave is superimposed by the hydropeaking regulation of both two dams. Hence the regulation time of the downstream Gezhouba dams has a significant influence on the flood wave propagation. If the regulation time is adjusted from the 0.6h to 1.2h, the flood wave amplitude will be significantly enhanced. The bottom friction has little effect on the wave height, but it will expedite the attenuation time of the flood wave during its propagation.

Key words: hydropeaking regulation, flood wave, analytical model, standing wave, energy attenuation

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