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长江万州至长寿河段泥沙淤积特性研究
引用本文:罗,宏.长江万州至长寿河段泥沙淤积特性研究[J].水运工程,2013(1):109-113.
作者姓名:  
作者单位:重庆交通大学河海学院,重庆400074;长江重庆航道工程局,重庆400011
摘    要:三峡水库蓄水后,库区河段泥沙淤积较蓄水前发生了较大变化。对三峡库区实测资料及多年库区冲淤变化分析表明:三峡库区的淤积形态与河型有关——弯曲河段和分汊河段淤积较为严重,顺直河段淤积相对较少。对长江万州至长寿河段典型河型进行冲淤分析,为进一步研究提供参考。

关 键 词:长江  万州至长寿河段  泥沙淤积

On sedimentation in the Yangtze River from Wanzhou to Changshou reach
LUO Hong.On sedimentation in the Yangtze River from Wanzhou to Changshou reach[J].Port & Waterway Engineering,2013(1):109-113.
Authors:LUO Hong
Institution:Chongqing Jiaotong University, Chongqing 400074, China;Changjiang Chongqing Waterway Engineering Bureau, Chongqing 400011, China
Abstract:After impoundment of the three Gorges reservoir, obvious changes took place on river bed evolution of the reach in the reservoir area. Based on an analysis of measured data and scour-and-fill variation for many years, we get to know that sediment deposition geometry relates to the river pattern: deposition at the bend or branch reach is serious while that at the straight reach is lower. The analysis presented on river bed evolution of typical river patterns in the upper Yangtze River from Wanzhou to Changjiang reach provides reference for further studies.
Keywords:the Yangtze River  reach from Wanzhou to Changshou  sedimentation
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