长江科学院院报 ›› 2025, Vol. 42 ›› Issue (2): 91-99.DOI: 10.11988/ckyyb.20231129

• 水力学 • 上一篇    下一篇

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 430010
    5 三峡大学 水利与环境学院,湖北 宜昌 443002
  • 收稿日期:2023-10-18 修回日期:2024-05-15 出版日期:2025-02-01 发布日期:2025-02-01
  • 通信作者:
    刘新波(1990-),男,山西大同人,工程师,博士,研究方向为梯级水库动力与环境过程。E-mail:
  • 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。E-mail:

  • 基金资助:
    国家自然科学基金项目(42477086); 国家自然科学基金项目(U24A20180); 国家自然科学基金项目(42006156); 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); 三峡创新发展联合基金项目(2023AFD201); 长江科学院开放研究基金项目(CKWV20221003/KY); 湖北省高校优秀中青年科技创新团队项目(T2021003); 湖北省自然科学基金项目(2022CFB207)

Characteristics of Flood Propagation in River between Two Dams Driven 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 EngineeringDesign Co.,Ltd.,Chongqing 400020,China
    3 Chongqing Construction Science Research Institute Co., Ltd.,Chongqing 400042,China
    4 River Research Department, Changjiang River Scientific Research Institute,Wuhan 430010, China
    5 College of Hydraulic and Environmental Engineering, China Three GorgesUniversity, Yichang 443002, China
  • Received:2023-10-18 Revised:2024-05-15 Published:2025-02-01 Online:2025-02-01

摘要:

基于三峡和葛洲坝电站2018年实测水位、流量数据和一维解析模型,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,2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在1 500~2 000 m3/s和1 200~1 500 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0.5~0.8 m之间。基于一维解析模型能够很好地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。河道底摩擦因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 measured water level and discharge data in 2018, this paper investigates the propagation of flood waves in the river reach between Three Gorges Dam and Gezhouba Dam driven by hydropeaking regulation by using a one-dimensional analytical model. During daily hydropeaking operations at both dams, the outflow exhibited significant diurnal and semi-diurnal fluctuations, ranging from 1 500 to 2 000 m3/s for Three Gorges Dam and 1 200 to 1 500 m3/s for Gezhouba Dam in average. Similarly, the water level at Huanglingmiao and Nanjinguan stations fluctuated by about 0.5-0.8 m daily. The one-dimensional analytical model accurately simulates the fluctuation of water level and discharge between the two dams. The simulation results indicate that flood waves in the river reach propagate as high-frequency standing waves with a period of 1.2 hours. The maximum amplitudes of the standing waves are approximately 2.1 cm for water level and 210 m3/s for flow discharge. The flood waves are superimposed by the hydropeaking operations of both dams, and the timing of regulation at Gezhouba Dam significantly affects flood wave propagation. Specifically, increasing the regulation time from 0.6 to 1.2 hours substantially enhances the flood wave amplitude. While bottom friction of river channel has a negligible impact on wave height, it accelerates the attenuation of flood waves during propagation.

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

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