首页 | 本学科首页   官方微博 | 高级检索  
     

天然河道不连续宽级配床沙特性及形成条件探讨
引用本文:魏丽,卢金友,徐海涛.天然河道不连续宽级配床沙特性及形成条件探讨[J].长江科学院院报,2012,29(10):6-10.
作者姓名:魏丽  卢金友  徐海涛
作者单位:1.中国科学院山地灾害与地表过程重点实验室, 成都610041; 2.中国科学院水利部成都山地灾害与环境研究所,成都 610041; 3.长江科学院,武汉430010
基金项目:国家自然科学基金(50879006);中国科学院知识创新工程重要方向项目群(KZCX2-YW-JS305)
摘    要:选取我国有代表性的几个河段对不连续宽级配床沙特性及形成条件进行了初步探讨,为不连续宽级配床沙运动规律研究提供了基础。认为不连续宽级配床沙特性为:泥沙粒径范围很宽,某一粒径范围泥沙较少甚至缺失,床沙粒径重量百分数具有明显的双峰分布特征。不连续宽级配床沙形成的一般条件为:河床床沙本身具有一定的不均匀性,河床有一定的覆盖层厚度,上游具有补给性的来沙条件,河段水流速度具有一定的变化幅度。

关 键 词:不连续宽级配床沙  床沙特性  床沙粒径  形成条件

Characteristics and Formation Conditions of Discontinuous Widely-Graded Sediment in Natural River Course
WEI Li , LU Jin-you , XU Hai-tao.Characteristics and Formation Conditions of Discontinuous Widely-Graded Sediment in Natural River Course[J].Journal of Yangtze River Scientific Research Institute,2012,29(10):6-10.
Authors:WEI Li  LU Jin-you  XU Hai-tao
Affiliation:1.Key Laboratory of Mountain Hazards and Earth Surface Processes, Chinese Academy of Sciences, Chengdu  610041, China;  2.Institute of Mountain Hazards and Environment, Chinese Academy of Sciences &; Ministry of Water Resources, Chengdu  610041, China; 3.Yangtze River Scientific Research Institute, Wuhan  430010, China
Abstract:With three typical natural river courses in China as case study,we preliminarily discussed the characteristics and formation conditions of discontinuous widely-graded sediment,providing basis for researching discontinuous widely-graded bed load transport.It’s believed that the characteristics of discontinuous widely-graded sediment are as follows:the sediment particle size varies in a wide range;sediment of a certain size is in a small amount or even in absence;and the weight percent of bed sediment exhibits a clear bimodal distribution.The formation of discontinuous widely-graded sediment is based on three conditions:non-uniform bed sediments and thick riverbed cover,sediment supplies from the upstream,and varying flow velocity in the river course.
Keywords:discontinuous widely-graded sediment  sediment characteristic  sediment particle size  formation condition
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《长江科学院院报》浏览原始摘要信息
点击此处可从《长江科学院院报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号