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库水位升降作用下大型堆积体边坡变形破坏预测
引用本文:董金玉,杨继红,孙文怀,黄志全,王东,杨国香.库水位升降作用下大型堆积体边坡变形破坏预测[J].岩土力学,2011,32(6):1774-1780.
作者姓名:董金玉  杨继红  孙文怀  黄志全  王东  杨国香
作者单位:1. 华北水利水电学院 资源与环境学院,郑州 450011;2. 中国科学院地质与地球物理研究所 中国科学院工程地质力学重点实验室,北京 100029
基金项目:华北水利水电学院高层次人才引进项目资助,中国科学院工程地质力学重点实验室开放基金项目资助,教育部留学回国人员科研启动基金资助
摘    要:库岸边坡的变形破坏及稳定性研究是目前国内外研究的热点之一。基于水电站库区一大型堆积体边坡,通过现场原位直剪试验获取岩土体的力学参数,利用岩土数值分析FLAC3D软件,考虑了堆积体与基岩基覆接触带介质的应变软化特性,对水库蓄水和下降过程中边坡的变形破坏特征进行了分析预测。结果表明,在库水升降作用下变形主要发生在堆积体内部;根据堆积体的变形特征可分为3个区:前缘牵引变形区,变形量最大;中间过渡区,变形量最小;后缘被牵引变形区,变形量介于前缘和中间之间。模拟过程中,在坡体的不同位置设置位移监测点,得到了蓄水和水位下降过程中各监测点的位移时程曲线,监测结果显示,水位下降时堆积体前缘易形成局部失稳。通过剪应变增量判断堆积体边坡在库水作用下可形成2个潜在的滑动破坏面

关 键 词:库水升降  堆积体边坡  应变软化  牵引变形区  破坏模式  局部失稳  
收稿时间:2010-02-03

Prediction of deformation and failure of a large-scale deposit slope during reservoir water level fluctuation
DONG Jin-yu,YANG Ji-hong,SUN Wen-huai,HUANG Zhi-quan,WANG Dong,YANG Guo-xiang.Prediction of deformation and failure of a large-scale deposit slope during reservoir water level fluctuation[J].Rock and Soil Mechanics,2011,32(6):1774-1780.
Authors:DONG Jin-yu  YANG Ji-hong  SUN Wen-huai  HUANG Zhi-quan  WANG Dong  YANG Guo-xiang
Institution:1. College of Resources and Environment, North China Institute of Water Conservancy and Hydroelectric Power, Zhengzhou 450011, China 2. Key Laboratory of Engineering Geomechanics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Abstract:Research on deformation and stability of reservoir bank slopes is one of the focus in the world.Taking a deposit slope in the hydropower reservoir area for example,the deformation and failure characteristics of the slope are predicted by FLAC3D while the reservoir level is rising and rapid drawdown.It is indicated that deformation mainly occurred in the deposit body while the reservoir level fluctuating;the deposit body is divided into three regions according to the deformation characteristics: the front tr...
Keywords:reservoir filling and rapid drawdown  deposit slope  traction deformation area  failure mode  local instability  
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