raybet体育在线 院报 ›› 2025, Vol. 42 ›› Issue (6): 8-13.DOI: 10.11988/ckyyb.20240324

• 河湖保护与治理 • 上一篇    下一篇

2023年下荆江湖南段“天字一号”护岸段崩岸分析

陈益民1(), 林荡1, 阳甜甜1, 郑保1, 张国华1, 李凌云2, 郭超2()   

  1. 1 岳阳市长江洞庭湖水利事务中心,湖南 岳阳 414000
    2 raybet体育在线 水利部长江中下游河湖治理与防洪重点实验室,武汉 430010
  • 收稿日期:2024-04-02 修回日期:2024-04-27 出版日期:2025-06-01 发布日期:2025-06-01
  • 通信作者:
    郭 超(1990-),男,湖北武汉人,高级工程师,博士,研究方向为河湖保护与治理。E-mail:
  • 作者简介:

    陈益民(1968-),男,湖南平江人,工程师,主要从事长江河势变化等研究。E-mail:

  • 基金资助:
    国家重点研发计划项目(2023YFC3209500); 湖南省水利科技项目(XSKJ2023059-58)

Analysis of Bank Collapse at “Tianzi-1” Revetment Section in Hunan Segment of Lower Jingjiang River in 2023

CHEN Yi-min1(), LIN Dang1, YANG Tian-tian1, ZHENG Bao1, ZHANG Guo-hua1, LI Ling-yun2, GUO Chao2()   

  1. 1 Yueyang Dongting Lake Water Conservancy Affairs Center, Yueyang 414000, China
    2 Key Laboratory of River and Lake Regulation and Flood Control in the Middle and Lower Reaches of Yangtze River of Ministry of Water Resources, Changjiang River Scientific Research Institute, Wuhan 430010, China
  • Received:2024-04-02 Revised:2024-04-27 Published:2025-06-01 Online:2025-06-01

摘要:

三峡工程及长江上游水库群建库运行以来,新水沙形势下荆江河段发生大范围、高强度持续冲刷,导致部分护岸工程段崩岸险情时有发生,对河势稳定、防洪安全及岸线利用等造成较大影响。以2023年下荆江已护险工段“天字一号”段突发崩岸险情及处置为例,通过实测资料分析,揭示了崩岸发生的主要原因为“清水下泄”情势下河床持续冲深、局部河势显著调整变化引起深泓深槽贴岸、河段岸坡地质条件较差以及持续中低水位影响等。基于险情特征,采取水下抛石方式对窝崩险工段及上下游影响段进行应急处置,提出亟需建立体制机制,保障相关建设资金,重视和加强对险工段坡脚变化的动态监测和整治技术研发,完善崩岸监测预警及应急抢护机制等中长期治理建议,为新水沙情势下长江中下游河道崩岸系统防治提供支撑。

关键词: 崩岸, 水沙情势, 河道演变, 险情处置, 荆江

Abstract:

[Objectives] Since the operation of the Three Gorges Project and the cascade reservoirs in the upper reaches of the Yangtze River, the new water and sediment regime has caused large-scale and high-intensity continuous erosion in the Jingjiang River section of the middle Yangtze River, resulting in recurrent bank collapse incidents at some revetment sections. To investigate the causes of recent bank collapses at revetment sections and better respond to such dangerous situations, this study examines the sudden bank collapse and its emergency treatment at the “Tianzi-1” revetment section in the lower Jingjiang River in 2023. [Methods] Measured water and sediment data at Jianli station since 1990, annual erosion and deposition data of the lower Jingjiang River since 2003, and measured data on channel topographic changes and geological drilling before and after the bank collapse at the “Tianzi-1” section were used to analyze the causes. [Results] In November 2023, continuous cave-in-type bank collapses occurred at the “Tianzi-1” revetment section in the Hunan segment of the lower Jingjiang River, with collapse lengths of approximately 100 m and 35 m, respectively. The results showed that the bank collapse primarily resulted from continuous riverbed erosion under the clear-water discharge condition, significant changes in local river regime causing deep channel and thalweg migration toward banks, poor geological conditions of the riverbank slope, and the influence of prolonged low-to-medium water levels. Based on the characteristics of the dangerous situation, an underwater stone dumping method was adopted for emergency treatment of the collapsed section and the affected upper and lower reaches. [Conclusions] This recurrent bank collapse at the revetment section highlights that the lower Jingjiang River will continue to face severe threats of bank collapse for the foreseeable future. Without timely reinforcement measures, large-scale damage can occur to existing bank protection structures, seriously threatening flood control safety. Therefore, this study proposes medium-to-long-term governance measures, including establishing institutional frameworks as soon as possible, securing construction funding, strengthening dynamic monitoring of slope toe variations at dangerous sections, enhancing the development of bank failure control technologies, and improving the monitoring, early warning, and emergency response mechanisms for bank collapse.

Key words: bank collapse, water and sediment regime, channel evolution, emergency treatment, lower Jingjiang River

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