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三峡建库后下荆江七弓岭至观音洲河弯段冲淤特征变化

姜梓璇 陈明洪 黄烈敏 李伟志 郑敬云 陈鑫

水力发电学报2026,Vol.45Issue(9):27-38,12.
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水力发电学报2026,Vol.45Issue(9):27-38,12.DOI:10.11660/slfdxb.20260903

三峡建库后下荆江七弓岭至观音洲河弯段冲淤特征变化

Changes in erosion and deposition characteristics of Qigongling-Guanyinzhou bend section in lower Jingjiang after construction of Three Gorges reservoir

姜梓璇 1陈明洪 1黄烈敏 2李伟志 1郑敬云 3陈鑫1

作者信息

  • 1. 中国农业大学 水利与土木工程学院,北京 100083
  • 2. 长江水利委员会 荆江水文水资源勘测局,湖北 荆州 434000
  • 3. 温州职业技术大学 建筑工程学院,浙江 温州 325000
  • 折叠

摘要

Abstract

Understanding the characteristics of erosion and deposition in river bends helps predict bank evolution,and guides flood control safety,efficient water resources utilization,and navigational channel maintenance.Erosion-deposition patterns in a river bend are typically characterized by concave erosion and convex deposition.However,following the Three Gorges Reservoir impoundment,multiple sharp bends in the lower Jingjiang River shifted to the anomalous pattern-convex erosion and concave deposition.This study examines this anomalous phenomenon through numerical simulations of erosion and deposition in the river section from the Qigongling bend to the Guanyinzhou bend in the lower Jingjiang under the conditions of multiple flow regimes.The results indicate that the reservoir operation leads to longer water flow duration and a sharp decrease in sediment inflow,causing the main flow axis to shift towards the convex bank and the river section to shift to the anomalous pattern.Under medium and high flow levels,the erosion zone is highly consistent with the high-velocity main channel.As the flow level rises,the mainstream path deviates towards the convex bank,and the erosion there intensifies accordingly.Sediment concentration and its variation play a regulatory role in erosion-deposition intensity.Under the same flow level,a significant decrease in the concentration strengthens erosion,while an increase promotes deposition.We have obtained the concentration thresholds as a switching condition between erosion and deposition under different flow levels.This study gives a preliminary clarification of the synergistic mechanism of flow level and sediment concentration underlying the spatial distribution and intensity of sedimentation,laying a basis for understanding the evolution of curved river channels downstream of reservoirs.

关键词

长江中游/冲淤变化/岸滩演变/流量/含沙量

Key words

middle Yangtze River/sediment transport dynamics/bank evolution/flow rate/sediment load

分类

建筑与水利

引用本文复制引用

姜梓璇,陈明洪,黄烈敏,李伟志,郑敬云,陈鑫..三峡建库后下荆江七弓岭至观音洲河弯段冲淤特征变化[J].水力发电学报,2026,45(9):27-38,12.

基金项目

国家重点研发计划(2022YFC3201804) (2022YFC3201804)

水力发电学报

1003-1243

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