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

水库蓄水过程中堆积体边坡瞬态稳定性分析
引用本文:杨继红,王俊梅,董金玉,刘汉东,王四巍.水库蓄水过程中堆积体边坡瞬态稳定性分析[J].岩土力学,2011,32(Z1):464-0470.
作者姓名:杨继红  王俊梅  董金玉  刘汉东  王四巍
作者单位:华北水利水电学院 资源与环境学院, 郑州 450011
基金项目:华北水利水电学院高层次人才引进项目(No.200902);河南省教育厅自然科学研究计划项目(No.2010B410002)
摘    要:由现场试验结合Fredlund和Xing方法确定了堆积体的非饱和渗透性函数分布曲线。根据概化的地质模型,建立了非饱和渗流分析的有限元模型,模拟得到蓄水过程中不同时刻坡体中孔隙水压力的分布。把暂态孔隙水压力的分布和非饱和土强度理论应用到普遍极限平衡法(GLE)中,进行了库水上升过程中边坡瞬态稳定性分析。结果表明,库水上升过程中,坡体整体稳定性是下降的,而在受库水变动影响的局部区域,其稳定性系数随着库水位的上升表现出先减小后增大的趋势,即存在一个危险水位,在一定条件下,可能会诱发坡体下部局部区域失稳。

关 键 词:水库蓄水  非饱和土  非饱和渗透系数  普遍极限平衡法  瞬态稳定性  
收稿时间:2010-12-14

Analysis of transient stability of deposits slope in process of reservoir impounding
YANG Ji-hong,WANG Jun-mei,DONG Jin-yu,LIU Han-dong,WANG Si-wei.Analysis of transient stability of deposits slope in process of reservoir impounding[J].Rock and Soil Mechanics,2011,32(Z1):464-0470.
Authors:YANG Ji-hong  WANG Jun-mei  DONG Jin-yu  LIU Han-dong  WANG Si-wei
Institution:Institute of Resources and Environment, North China Institute of Water Conservancy and Hydroelectric Power, Zhengzhou 450011, China
Abstract:Unsaturated hydraulic conductivity functions of deposits body are obtained based on Fredlund and Xing methods as well as field tests. According to the generalized geological model, the finite element model of unsaturated seepage analysis is built. Distribution characteristics of pore-water pressure in the slope at different times in the process of reservoir impounding are obtained by numerical simulation. Distribution of transient pore-water pressure and the strength theory of unsaturated soil are applied to the analysis of general limit equilibrium to study the transient stability of the slope while the water level is rising. The results show that the whole stability of the slope is descending with the water level rising. And its local stability coefficient is descended firstly and then ascended with the reservoir water level rising. Owing to the existence of a risk water-level, the lower part of slope body tends to be unstable under certain condition
Keywords:eservoir filling  unsaturated soil  unsaturated hydraulic conductivity  general limit equilibrium method  transient stability  
本文献已被 CNKI 等数据库收录!
点击此处可从《岩土力学》浏览原始摘要信息
点击此处可从《岩土力学》下载免费的PDF全文
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