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汉江库区变动回水区铁板沙的观测与分析
引用本文:胡家庆,章厚玉,柳发忠.汉江库区变动回水区铁板沙的观测与分析[J].长江工程职业技术学院学报,2005,22(2):22-24.
作者姓名:胡家庆  章厚玉  柳发忠
作者单位:长江水利委员会汉江水文水资源勘测局,湖北,丹江口,442700;长江水利委员会汉江水文水资源勘测局,湖北,丹江口,442700;长江水利委员会汉江水文水资源勘测局,湖北,丹江口,442700
摘    要:铁板沙是汉江库区变动回水区的一种泥沙淤积现象,是沙浪、沙垄运动的产物.根据实测资料分析,得出了铁板沙的形成必须同时满足的两个条件,一是粒径在0.1~0.5mm的中细沙占80%以上;二是床面流速需大于2.0m/s.为进一步研究铁板沙的形成与治理提供参考.

关 键 词:汉江  淤积  铁板沙  分析
文章编号:1673-0496(2005)02-0022-03
修稿时间:2004年10月9日

Survey and Analysis of Consolidated Sand in Varying Backflow Zone of Hanjiang Reservoir
HU Jia-qing,ZHANG Hou-yu,LIU Fa-zhong.Survey and Analysis of Consolidated Sand in Varying Backflow Zone of Hanjiang Reservoir[J].Journal of Changjiang Engineering Vocational College,2005,22(2):22-24.
Authors:HU Jia-qing  ZHANG Hou-yu  LIU Fa-zhong
Abstract:Consolidated sand, caused by the movement of sand wave and longitudinal dune, is a silting phenomenon takes place in backflow zone of Hanjiang Reservoir. According to the data from on-the-spot survey, to form the consolidated sand two conditions that 80 percent of sand diameter must between 0.1mm and 0.5 mm and that the speed of top river must be above 2.0m/s have to be met at the same time.
Keywords:Hanjiang River  silting  consolidated sand  analysis
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