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白鹤滩水库场次洪水特征分析

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基于2015-2022年白鹤滩库区实测水沙资料,划分白鹤滩水库场次洪水过程,分析了白鹤滩水库运行前后汛期场次洪水的水沙运动特点变化情况。结果表明:白鹤滩入库泥沙集中于汛期场次洪水,受上游水库拦沙影响,干流洪水输沙量显著减少,泥沙主要来自库区区间。出入库洪峰流量以7 500~12 500 m3/s为主,该流量级洪水输沙量占比超58%;出入库洪水均以沙峰超前洪峰为主,含沙量-流量曲线以顺时针为主。乌东德和白鹤滩水库运行前,汛期河段入口洪水洪峰沙峰值均较高,由于河段区间产沙沿程补给,河段出口沙量高于入库沙量;乌东德和白鹤滩水库运行后,汛期出入库洪水洪峰沙峰减小,沙峰坦化现象突出。
Analysis of flood characteristics in the Baihetan Reservoir
Based on the measured water and sediment data in the Baihetan Reservoir from 2015 to 2022,the flood processes were divided,and the characteristics of the flood and sediment transport during flood seasons before and after the operation of Baihetan Reservoir have been analyzed.The results show that the sediment in Baihetan Reservoir concentrates in flood seasons,and the sediment transported by the main stream flood reduces significantly due to the influence of the upstream reservoir.The peak discharge entering and exiting the reservoir is mainly of 7 500~12 500 m3/s,and the sediment transport volume in this flow rate level accounts for more than 58%.The relationship curves of sediment concentration andflow rate are mainly clockwise,which means the sediment peak get ahead the flood peak during floods entering and exiting the reservoir.Before the operation of the Wudongde Reservoir and Baihetan Reservoir,the flood peak and sediment peak are higher in flood season,and the incoming sediment concentration is generally higher than that exiting the reservoir with the sediment replenishment along the reservoir area.After the operation of Wudongde and Baihetan reservoirs,the flood peak and sediment peak decrease and the sediment peak get flattening obviously.

Baihetan Reservoirflood eventincoming flow and sedimentflood and sediment peaks

吕瑞茹、邓安军、张帮稳、陈翠华、路子岩

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中国水利水电科学研究院流域水循环模拟与调控国家重点实验室,北京 100048

中国水利水电科学研究院水利部泥沙科学与北方河流治理重点实验室,北京 100048

中国长江电力股份有限公司智慧长江与水电科学湖北省重点实验室,湖北宜昌 443000

白鹤滩水库 场次洪水 入库水沙 洪峰沙峰

2024

泥沙研究
中国水利学会

泥沙研究

CSTPCD北大核心
影响因子:0.817
ISSN:0468-155X
年,卷(期):2024.49(6)