中文核心期刊
CSCD来源期刊
中国科技核心期刊
RCCSE中国核心学术期刊

Journal of Chongqing Jiaotong University(Natural Science) ›› 2011, Vol. 30 ›› Issue (6): 1384-1387.DOI: 10.3969/j.issn.1674-0696.2011.06.29

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Variety Characteristics of Sediment Size in Wanzhou-Lidu Reach during 135 - 139m Water Phase of the Three Gorges Reservoir

YANG Sheng-fa,WANG Xiao,HU Jiang   

  1. School of River & Ocean Engineering,Chongqing Jiaotong University,Chongqing 400074,China
  • Received:2011-06-10 Revised:2011-07-01 Online:2011-12-15 Published:2015-01-22

三峡水库135~139 m 蓄水阶段 万州—李渡河段床沙粒径变化特性

杨胜发,王筱,胡江   

  1. 重庆交通大学河海学院,重庆400074
  • 作者简介:杨胜发(1970—),男,四川邻水人,教授,博士后,主要从事航道整治方面研究。E-mail:yuangd666@126.com。

Abstract: From Jun. 2003 to Sep. 2006,the Three Ggorges Reservoir is running with the 135—139 m dispatching operation scheme. The scheme means the water level is 139m during low water season and 135m during flood season. The backwater end is located at Lidu in Fuling district,and the reach ever in back water is below Fengdu. Through analyzing the prototype observation data of the Three Gorges Reservoir,the variety characteristics and the gradation of sediment in this reach has been studied. The rule of sediment motion is obtained based on the analysis of sediment size in this reach,which could be a preliminary understanding of sediment motion rule in the Three Gorges Reservoir district.

Key words: the Three Gorges Reservoir, river bed sediment, deposit, sediment motion

摘要: 从2003 年6 月—2006 年9 月三峡水库库水位按135 ~ 139 m 方式运行( 枯水期坝前水位139 m,汛期坝前水位 135 m) ,其回水末端位于涪陵李渡附近,常年库区在丰都以下。分析了该阶段蓄水期三峡库区原型观测资料,研究 了万州—涪陵李渡河段床沙沿程变化特性及淤积物的级配组成,由该河段的床沙粒径变化分析其泥沙基本运动规 律,从而对该河段以至于三峡库区的泥沙运动规律有一个初步的认识。

关键词: 三峡水库, 床沙, 淤积物, 泥沙运动

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