水利水电科技进展2011，Vol.31Issue(2)：23-27,5.DOI:10.3880/j.issn.1006-7647.2011.02.006
黄河尾闾河道平滩流量变化对来水来沙的响应
Response of bankfull discharge in tail reaches of Yellow River estuary to runoff and sediment load
摘要
Abstract
By analvzing the characteristics of erosion-deposition variation and channel shrinkage in the tail reaches of Yellow River estuary since the tail reaches of Yellow River estuary changed to Qingshuigou flow path in 1976, the relationship between the bankfull discharge at Lijin station and the incident runoff and sediment as well as the extension of river length was studied. The results show that the bankfull discharge in tail reaches of Yellow River estuary relates with the runoff volume, flood peak discharge, coefficient of water and sediment, channel length and preceding bed-channel conditions. The quantitative relationship among the water volume, the peak discharge and the coefficient of the water and the sediment load for the bankfuil discharge of 4000m3/s as well as the restriction conditions for the channel length is proposed. It may provide a reference for the integrated management of tail reaches.关键词
黄河河口河道/冲淤变化/平滩流量/来水量/水沙搭配系数/河口河长/响应关系Key words
tail reach of Yellow River estuary/ eresion-deposition variation/ bankfull discharge/ runoff volume/ coefficient of water and sediment/ channel length/ response relation分类
天文与地球科学引用本文复制引用
侯志军,李勇,庞隆霞..黄河尾闾河道平滩流量变化对来水来沙的响应[J].水利水电科技进展,2011,31(2):23-27,5.基金项目
水利部公益性行业科研专项(200701036) （200701036）
中央级公益性科研院所基本科研业务(HKY-JBYW-2008) （HKY-JBYW-2008）
