首页 | 本学科首页   官方微博 | 高级检索  
     检索      

三峡库区土脑子河段冲淤特性分析
引用本文:张强.三峡库区土脑子河段冲淤特性分析[J].长江工程职业技术学院学报,2006,23(3):16-18.
作者姓名:张强
作者单位:长江上游水文局,宜宾水文勘测队,四川,宜宾,644007
摘    要:土脑子河段处在三峡工程135m运行水位的变动回水区,天然情况下具有汛期淤积、汛末及汛后冲刷、年内冲淤平衡的规律.三峡工程蓄水以来,河段洲滩、岸线无明显变化,河床冲淤主要集中在右侧主槽土脑子一带.由于汛期淤沙在汛末、汛后及次年消落期冲刷不足,河段产生了累积性淤积.分析表明,水库调度、来水来沙、河床形态是影响冲淤变化的主要因素.

关 键 词:土脑子河段  冲淤变化  变动回水区  三峡工程
文章编号:1673-0496(2006)03-0016-03
收稿时间:2006-04-11
修稿时间:2006年4月11日

Analysis of Aggradation and Degradation of Tunaozi Reach in Three Gorges Reservoir Area
ZHANG Qiang.Analysis of Aggradation and Degradation of Tunaozi Reach in Three Gorges Reservoir Area[J].Journal of Changjiang Engineering Vocational College,2006,23(3):16-18.
Authors:ZHANG Qiang
Institution:Yibin Surveying Team of Changjiang Upper Reaches Hydrological Bureau, Yibin, Sichuan 644007, China
Abstract:The Tunaozi reach, which lies in the 135m fluctuant backwater area of the Three Gorges Project, under natural condition, has the characteristics of aggradation during flood season, scouring in late flood season and after flood season and balanced aggradation and scouring in a year. Since the Three Gorges reservoir begarrto store water, the fiver bank of the reach has not changed clearly and the river bed scour has been discovered mainly on the fight trough. Because of the sediment during the flood season and the uneven scour after flood season and the following year, accumulated sediment arises. Analysis shows that the adjustment of the reservoir, the coming water and sand, and the form of the fiver bed are the main factors of sediment change.
Keywords:Tunaozi reach  aggradation and degradation  fluctuant backwater area  Three Gorges Project
本文献已被 CNKI 维普 万方数据 等数据库收录!
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