人民长江 ›› 2021, Vol. 52 ›› Issue (12): 1-8.doi: 10.16232/j.cnki.1001-4179.2021.12.001

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2020年长江中下游干流河道冲淤变化特点及分析

许全喜;董炳江;张为   

  • 发布日期:2022-01-10

Characteristics and analysis on scouring and silting changes in main stream of middle and lower reaches of Changjiang River in 2020

XU Quanxi, DONG Bingjiang,ZHANG Wei   

  • Published:2022-01-10

摘要: 2020年汛期长江流域出现了历时长、范围广的强降雨过程,发生了新中国成立以来仅次于1954,1998年的罕见大洪水。基于现有资料,对2020年大洪水条件下长江中下游干流河道的冲淤变化特点进行了分析。结果表明:上游来沙和三峡水库出库泥沙明显增多是造成宜昌至湖口河段河床冲刷量偏小的原因之一,同时中下游干流洪水顶托严重,减小了宜昌至湖口河道的输沙能力;汛期长江中下游干流涨水较快,易造成河道泥沙落淤,汛后退水慢,河道泥沙得不到有效冲刷。湖口至江阴江段水面比降大,加之河道含沙量低,造成冲刷量偏大。研究成果为进一步深入研究长江中下游河道冲淤变化规律和未来冲淤趋势预测提供了基础和参考依据。

关键词: 水库群; 多目标联合调度; 全周期建模; 长江流域;

Abstract: In the flood season of 2020,there was a long-lasting and wide-ranging heavy rainfall process in the Changjiang River Basin,which was only less than flood in 1954 and 1998 flood since 1949. We analyzed the scouring and silting change characteristics of the main stream of the middle and lower reaches of the Changjiang River under the 2020 flood. The results showed that the increase of upstream sediment and discharge sediment of Three Gorges Reservoir led to the decrease of scouring in the reach of Yichang to Hukou,and at the same time the severe backwater effect at middle and lower reach also reduced the sediment transport ability of this reach. During the flood,the water level rose quickly in the middle and lower reach,leading to easy silting,however the water fell slowly after the flood,causing un-sufficient scouring of sediment in the reach. In the Hukou to Jiangyin reach near the estuary,the water gradient was large and with less sediment concentration,so the sediment transport was relative large. The research provides a basis and reference for further study on the change law of scouring and silting in the middle and lower reaches of the Changjiang River and the prediction of scouring and silting trend in the future.

Key words: river channel scouring and silting; flood jacking; Changjiang River flood in 2020; middle and lower reaches of the Yangtze River;