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基于突变理论的黄河下游游荡性河道演变稳定性分析

曹智伟 宗虎城 李坤 樊金生 陆永军 肖洋 刘怀湘

水科学进展2026,Vol.37Issue(3):528-539,12.
水科学进展2026,Vol.37Issue(3):528-539,12.DOI:10.14042/j.cnki.32.1309.2026.03.011

基于突变理论的黄河下游游荡性河道演变稳定性分析

Stability analysis on channel evolution of a braided reach in the Lower Yellow River based on cusp catastrophe theory

曹智伟 1宗虎城 1李坤 2樊金生 3陆永军 4肖洋 5刘怀湘4

作者信息

  • 1. 黄河勘测规划设计研究院有限公司,河南郑州 450003||水利部黄河流域水治理与水安全重点实验室,河南郑州 450003
  • 2. 黄河勘测规划设计研究院有限公司,河南郑州 450003||河海大学水利部水循环与水动力系统重点实验室,江苏南京 210098
  • 3. 周口师范学院,河南周口 466001
  • 4. 南京水利科学研究院水灾害防御全国重点实验室,江苏南京 210029
  • 5. 河海大学水利部水循环与水动力系统重点实验室,江苏南京 210098||苏州科技大学环境科学与工程学院,江苏苏州 215009
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摘要

Abstract

This study focuses on the braided reach of the Lower Yellow River(LYR),which features abrupt and random river regime evolution.Studying such river regime stability variations and dominant controlling factors is crucial for addressing challenges such as channel braiding and flood control.Using the cusp catastrophe theory,this study takes thalweg migration intensity and flow scouring intensity as control variables to quantitatively analyze river regime stability in a typical braided reach before and after the operation of the Xiaolangdi Reservoir.The results show that river regime stability exhibited an overall increasing trend from 1992 to 2020.Before 2006,the river regime had been in a persistently unstable state,whereas after 2006,it shifted markedly to a stable state under water-sediment regulation,demonstrating the remarkable effect of altered water-sediment regimes on enhancing channel stability following the operation of the Xiaolangdi Reservoir.It was also found that the stability coefficient was significantly positively correlated with average scouring intensity and negatively correlated with thalweg migration intensity,where the discharge and sediment conditions constituted the dominant controlling factors.The results also indicate that after reservoir operation,average scouring intensity continuously increased,while thalweg migration width and intensity decreased significantly,leading to a substantial reduction in channel braiding.In addition,sediment concentration in flood seasons was the key factor affecting river regime stability as higher sediment concentration led to lower scouring intensity,greater thalweg migration intensity,and thus decreased river regime stability.Based on these findings,this study reveals the mechanism of stability variations in braided channel evolution driven by water-sediment regime changes,and provides theoretical support for water-sediment regulation and systematic governance of the LYR.

关键词

河道稳定性/游荡性河道/尖点突变理论/黄河下游

Key words

channel stability/braided channel/cusp catastrophe theory/the Lower Yellow River

分类

建筑与水利

引用本文复制引用

曹智伟,宗虎城,李坤,樊金生,陆永军,肖洋,刘怀湘..基于突变理论的黄河下游游荡性河道演变稳定性分析[J].水科学进展,2026,37(3):528-539,12.

基金项目

国家重点研发计划项目(2023YFC3208601) (2023YFC3208601)

国家自然科学基金项目(U2443220) The study is financially supported by the National Key R&D Program of China(No.2023YFC3208601)and the National Natural Science Foundation of China(No.U2443220). (U2443220)

水科学进展

1001-6791

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