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大渡河干海子滑坡稳定性研究
引用本文:杨智勇,吉锋.大渡河干海子滑坡稳定性研究[J].防灾减灾工程学报,2011,31(2):201-206.
作者姓名:杨智勇  吉锋
作者单位:浙江华东建设工程有限公司;成都理工大学地质灾害防治与地质环境保护国家重点实验室;
摘    要:干海子滑坡位于大渡河流域,规模巨大.为研究该滑坡的稳定性,在对滑坡基本特征及变形破坏特征等深入研究的基础上,采用极限平衡法(Geo-slope软件)和有限差分法(FLAC-3D软件)对该滑坡的稳定性和应力应变特征进行了计算、模拟.稳定性计算模拟主要从深层、浅层及局部稳定三方面入手分析,计算模拟结果与滑坡的宏现地质现象均...

关 键 词:大渡河  干海子滑坡  极限平衡法  有限差分法  稳定性研究

Research on Stability of Ganhaizi Landslide in Dadu River Basin
YANG Zhi-yong,JI Feng.Research on Stability of Ganhaizi Landslide in Dadu River Basin[J].Journal of Disaster Prevent and Mitigation Eng,2011,31(2):201-206.
Authors:YANG Zhi-yong  JI Feng
Institution:YANG Zhi-yong1,JI Feng2(1.East China Construction Engineering Corporation of Zhejiang,Hangzhou 310030,China,2.State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology,Chengdu 610059,China)
Abstract:Ganhaizi landslide is located in Dadu River Basin,which has large scale volume.In order to study the stability of the landslide,on the basis of researching the basic characteristics,deformation and failure of the landslide,its stability and stress-strain features were then calculated and analyzed by limit equilibrium method and finite difference method,which mainly analyze landslide′s deformation features from the respect of the deep layer,shallow layer and local stability. The results of the analysis are in line with the macro-geological phenomena.Through qualitatively and quantitatively analytic judgements,it is shown that the shallow sliding body in the storm conditions will be in the state of limit equilibrium,and deep sliding body in seismic condition will still be in the basic steady state.The result obtained will provide a reliable basis for the future landslide prevention work.
Keywords:Dadu River  Ganhaizi landslide  limit equilibrium method  finite difference method(FDM)  stability study  
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