摘要
在长江上游及中下游其他水系大型控制性水利枢纽建设和运行的综合影响下,进入长江下游的水沙条件显著变化,从而引起下游大通至江阴河段河床的冲淤调整。2001—2021年,大通至江阴河段河床趋势性的普遍冲刷较为明显,进而给沿江涉水工程的运行带来一定影响。以大通至江阴河段的水文、泥沙、固定断面及水下地形等观测数据为依据,对大通至江阴河段的水沙条件、河床冲淤量开展分析计算。
Under the comprehensive influence of the construction and operation of large-scale control water conservancy projects in the upper and middle Yangtze River,the water and sediment conditions entering the lower reaches of the Yangtze River have changed significantly,causing the scouring and silting adjustment of the riverbed of the downstream reach from Datong to Jiangyin.From 2001 to 2021,the trend of general erosion of the riverbed from Datong to Jiangyin is more obvious,which has a certain impact on the operation of wading projects along the river.Based on the observation data of hydrology,sediment,fixed cross-section and underwater topography of the Datong Jiangyin river section,the water and sediment conditions and the amount of riverbed scouring and siltation of the Datong Jiangyin river section are analyzed and calculated.
作者
朱玲玲
罗龙洪
曹双
ZHU Lingling;LUO Longhong;CAO Shuang(Yangtze River Water Conservancy Commission Hydrology Bureau,Wuhan 430010,China;Jiangsu Water Conservancy Project Planning Office,Nanjing 210029,China;Hydrology and Water Resources Investigation Bureau in the Lower Reaches of the Yangtze River,Nanjing 210011,China)
出处
《江苏水利》
2022年第10期58-62,共5页
Jiangsu Water Resources
基金
江苏省水利科技项目(2020001)
长江水科学研究联合基金(U2240224)。
关键词
长江下游
大通站
水沙条件
河床冲淤
The Lower reaches of the Yangtze River
Datong station
water and sediment conditions
scouring and silting of riverbed