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洪水位变化对岸滩稳定性的影响
引用本文:王延贵,匡尚富,陈吟.洪水位变化对岸滩稳定性的影响[J].水利学报,2015,46(12):1398-1405.
作者姓名:王延贵  匡尚富  陈吟
作者单位:国际泥沙研究培训中心, 北京 100048;中国水利水电科学研究院, 北京 100038,国际泥沙研究培训中心, 北京 100048;中国水利水电科学研究院, 北京 100038,北京交通大学, 北京 100044
基金项目:国家自然科学基金项目(51179208);十二五国家科技支撑计划资助项目(2012BAB04B02-2);中国水利水电科学研究院专项(沙基本科研1438)
摘    要:为了较全面地了解洪水涨落对岸滩崩塌的影响,本文通过对洪水期岸滩受力分析,结合岸滩土体性质和洪水浸泡岸滩特点,给出洪水期岸滩稳定系数;进而分析了洪水降落期岸滩稳定性变化,指出洪水骤降时,长期洪水浸泡后黏土岸滩稳定系数将会大幅度减小;在洪水缓慢降落时,黏性岸滩稳定性减小,但减小幅度小于骤降的情况。通过分析对比洪水上涨、洪水浸泡和洪水降落等不同过程的稳定性,指出洪水迅速上涨期岸滩稳定性最好,依次为洪水缓慢上涨期、洪水浸泡期和洪水缓慢下降期,洪水骤降期岸滩稳定性最差。

关 键 词:洪水位变化  洪水下降  稳定系数  岸滩崩塌
收稿时间:2015/4/29 0:00:00

Impacts of water level fluctuations on bank stability during flood period
WANG Yangui,KUANG Shangfu and CHEN Yin.Impacts of water level fluctuations on bank stability during flood period[J].Journal of Hydraulic Engineering,2015,46(12):1398-1405.
Authors:WANG Yangui  KUANG Shangfu and CHEN Yin
Affiliation:International Research and Training Center on Erosion and Sedimentation(IRTCES), Beijing 100048, China;China Institute of Water Resources and Hydropower Research(IWHR), Beijing 100038, China,International Research and Training Center on Erosion and Sedimentation(IRTCES), Beijing 100048, China;China Institute of Water Resources and Hydropower Research(IWHR), Beijing 100038, China and Beijing Jiaotong University, Beijing 100044, China
Abstract:In order to more fully understand the impacts of flood fluctuations on bank collapse, the bank stability coefficient during the flood period is given through the force analysis of the bank body, with con- sidering the soil properties and flood immersion characteristics of the river bank, and the bank stability changes in the process of the flood drop are further analyzed in this paper. It is pointed out that the stabili- ty coefficient of the clay bank with long-term flood immersion will decrease greatly after the flood falling. The stability coefficient of viscous bank will decrease during the flood slow recession period,but it is less than the flood falling. Through comparing stability coefficients in the different periods such as flood rising, flood immersion and flood recession, it is indicated that the bank stability is the best during the process of rapid flood rising, followed by the periods of flood rising slowly, the flood immersion and flood slow re- cession weakened in turn,and the worst bank stability is that during the flood descending period.
Keywords:flood water level changes  flood recession  stability coefficient  bank failure
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