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三峡建库后洞庭湖入汇对下荆江顶托特征的变化分析

李芷晴 孙昭华 陈立 安姗姗 周炜兴

水利学报2026,Vol.57Issue(5):767-781,15.
水利学报2026,Vol.57Issue(5):767-781,15.DOI:10.3724/j.slxb.20250601

三峡建库后洞庭湖入汇对下荆江顶托特征的变化分析

Changes in the backwater effect of Dongting Lake inflows on the Lower Jingjiang River after the impoundment of the Three Gorges Reservoir

李芷晴 1孙昭华 2陈立 2安姗姗 2周炜兴2

作者信息

  • 1. 武汉大学 水资源工程与调度全国重点实验室,湖北 武汉 430072||长江勘测规划设计研究有限责任公司,湖北 武汉 430010||流域水安全保障湖北省重点实验室,湖北 武汉 430010
  • 2. 武汉大学 水资源工程与调度全国重点实验室,湖北 武汉 430072
  • 折叠

摘要

Abstract

Clarifying the new characteristics of Dongting Lake's backwater effect on the lower Jingjiang River after the impoundment of the Three Gorges Reservoir is a critical issue at present.Focusing on the river section from Jianli to Chenglingji upstream of the confluence between the river and the lake,Copula functions were employed to investi-gate the characteristics of flow coincidences between the river and the lake in different periods.Based on the flow dynamics of alluvial rivers,a balanced-state flow pairing relationship was proposed,and an index for assessing the backwater intensity of the mainstream was developed.On this basis,the occurrence probability and timing of backwa-ter events as well as the variation of backwater intensity during different periods within a year for the lower Jingjiang River before and after the impoundment of the Three Gorges Reservoir were quantitatively analyzed.The results indi-cate that,under the balanced state,the flow pairing between the river and the lake follows a nonlinear functional rela-tionship.This relationship is close to the long-term mean fitted line of river-lake discharges and can be used to deter-mine whether the mainstream is in a backwater or drawdown state.After the impoundment of the Three Gorges Reser-voir,the duration of Jianli discharges at the medium-low flow level increased,resulting in a 44.6%rise in the coinci-dence probability of both the mainstream and lake inflows being at medium-low flow.The coincidence probability of the mainstream at medium flow and lake inflows at flood level(exceeding 30,000 m³/s)increased by 5.4%.As a result,the erosional base level at the river-lake confluence decreased,and on an annual scale,the mean backwater intensity of the lake on the mainstream weakened.However,the timing of the mainstream being in a backwater state shifted from above-bankfull flow levels to medium flow levels.The occurrence of extreme backwater intensity far exceeding the historical values during April-July has increased,warranting long-term attention.

关键词

三峡水库/下荆江/洞庭湖/流量遭遇/回水顶托

Key words

Three Gorges Reservoir/lower Jingjiang River/Dongting Lake/flow encounter/backwater effect

分类

建筑与水利

引用本文复制引用

李芷晴,孙昭华,陈立,安姗姗,周炜兴..三峡建库后洞庭湖入汇对下荆江顶托特征的变化分析[J].水利学报,2026,57(5):767-781,15.

基金项目

国家自然科学基金项目(52479074) (52479074)

水利部三峡后续研究项目(12630100100020J005) (12630100100020J005)

水利学报

0559-9350

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