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

水位涨落对库岸滑坡孔隙水压力影响的非饱和渗流分析
引用本文:柳群义,朱自强,何现启,鲁光银,唐军峰.水位涨落对库岸滑坡孔隙水压力影响的非饱和渗流分析[J].岩土力学,2008,29(Z1):85-89.
作者姓名:柳群义  朱自强  何现启  鲁光银  唐军峰
作者单位:1. 中南大学,资源与安全工程学院,长沙,410083
2. 中南大学,资源与安全工程学院,长沙,410083;中国水电工程顾问集团公司中南勘测设计研究院,长沙,410014
摘    要:以某水库库岸滑坡为工程背景,根据饱和-非饱和渗流控制方程,针对不同滑坡体渗透性和库水位升降速率,研究库水位变化条件下滑坡体内孔隙水压力的动态响应,得到:(1 水位升降时,在相同的入渗条件下,饱和渗透系数对初始地下水位有明显的影响;增大饱和渗透系数能降低地下水位,使地下水位线变得平缓,滑坡体的动、静水压力减小,有利于稳定;(2 增加库水位升降速率,地下水位响应滞后变得显著,地下水位线形态整体变陡,滑坡体的动水压力增大,不利于边坡稳定性.

关 键 词:水位涨落  库岸边坡  孔隙水压力  非饱和渗流
收稿时间:2008-07-25

Unsaturated seepage analysis of the influence of water level fluctuation on pore water pressure of landslide in reservoir area
LIU Qun-yi,ZHU Zi-qiang,HE Xian-qi,LU Guang-yin,TANG Jun-feng.Unsaturated seepage analysis of the influence of water level fluctuation on pore water pressure of landslide in reservoir area[J].Rock and Soil Mechanics,2008,29(Z1):85-89.
Authors:LIU Qun-yi  ZHU Zi-qiang  HE Xian-qi  LU Guang-yin  TANG Jun-feng
Institution:1. School of Info-physics and Geomatics Engineering, Central South University, Changsha 410083, China; 2. School of Resources & Safety Engineering, Central South University, Changsha, 410083, China; 3. Central South Design and Research Institute, CHECC Changsha 410014, China
Abstract:Iandslide in a certain reservoir area is chosen as the engineering background.According to the saturated-unsaturated seepage equation,the dynamic response of pore water pressure in the landslide influenced by the fluctuation of water level is studied when considering the infiltration characteristics and the fluctuation velocity of water level.The analysis results show that(1) when the water level fluctuates,the saturated permeability coefficient has great impact on the initial water level under the same inf...
Keywords:water level fluctuation  slope at reservoir area  pore water pressure  unsaturated seepage  
本文献已被 CNKI 万方数据 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