荆江河段水沙条件与主流线特征关系研究

刘亚; 李义天; 孙昭华; 陈飞

引用本文:	刘亚,李义天,孙昭华,陈飞.荆江河段水沙条件与主流线特征关系研究[J].水利水运工程学报,2011,(2):

【打印本页】【HTML】【下载PDF全文】【查看/发表评论】【EndNote】【RefMan】【BibTex】

←前一篇|后一篇→

过刊浏览高级检索

本文已被：浏览 943次下载 729次
分享到：微信更多字体:加大+\|默认\|缩小-
荆江河段水沙条件与主流线特征关系研究
刘亚¹,李义天²,孙昭华²,陈飞³
1. 长江科学院,湖北武汉,430010 2. 武汉大学水资源与水电工程科学国家重点实验室,湖北武汉,430072 3. 长江航道规划设计研究院,湖北武汉,430011

摘要:

荆江河段的主流变化主要表现为弯曲分汊段的主支汉交替及单一弯道段深泓半径的变化,综合考虑两者关系,提出了能描述荆江分汉段及单一弯道段主流线特点的无量纲常数--弯曲特征数r,并针对同一河段分析了汛期平均流量、洪峰变差系数、年输沙量及输沙指数等水沙条件变化与主流线变化的对应关系.结果表明:汛期平均流量较小、水流相对饱和度低、来水来沙过程较为均匀使得滩槽高差较小,横断面向宽浅发展,从而减弱河道对水流的约束,弯曲特征数较小,主流顺直;反之主流向弯曲发展.

关键词: 河床演变水沙条件水流动力轴线荆江河段

DOI：

分类号:TV147

基金项目:国家自然科学基金

Relationship between flow and sediment regime and changes of main streamline in Jingjiang reach

LIU Ya¹,LI Yi-tian²,SUN Zhao-hua²,CHEN Fei³

LIU Ya1,LI Yi-tian2,SUN Zhao-hua2,CHEN Fei3(1.Changjiang River Scientific Research Institute,Wuhan 430010,China,2.State Key Laboratory of Water Resources and Hydropower Engineering Science,Wuhan University,Wuhan 430072,2.Changjiang Waterway Planning,Design and Research Institute,Wuhan 430011,China)

Abstract:

The main streamline of Jingjiang reach changes in the form of alternation of main & tributary branches and radius of thalweg in bends.To describe the characteristics of mainstream line in bifurcated and curved reaches,this paper presents a dimensionless coefficient: sinuosity eigenvalue r.Correlation between r and other eigenvalues(such as dispersion of flood flow,sediment transport index,etc.) obtained by hydrological statistics reveals that less of average flood,uniformity of flow and incoming sediment wi...

Key words: fluvial process flow and sediment regime main streamline Jingjiang reach