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蒋家沟流域松散砾石土斜坡滑坡频发原因与试验模拟
引用本文:胡明鉴,汪稔,张平仓. 蒋家沟流域松散砾石土斜坡滑坡频发原因与试验模拟[J]. 岩石力学与工程学报, 2002, 21(12): 1831-1834
作者姓名:胡明鉴  汪稔  张平仓
作者单位:中国科学院武汉岩土力学研究所岩土力学重点实验室,武汉,430071
摘    要:降雨对滑坡的激发是广泛讨论的话题,从物质成分,结构构造和雨强,降雨量、土体应力特征等方面分析滑坡频发的原因,进行大型人工降雨 滑坡试验,观测降雨激发滑坡的过程,室内土工实验表明内聚力和内摩擦角与含水量之间有突变现象,松散砾石土斜滑坡是在以降雨为主导因素的多种因素综合作用下发生的。

关 键 词:蒋家沟流域 松散砾石土 斜坡 滑坡 试验模拟 降雨 滑坡 含水量 应力特征 突变
文章编号:1000-6915(2002)12-1831-04
修稿时间:2001-01-09

CAUSE OF FREQUENT OCCURRENCE OF GRAVEL SLOPE LANDSLIDE AND EXPERIMENT SIMULATION
Hu Mingjian,Wang Ren,Zhang Pingcang. CAUSE OF FREQUENT OCCURRENCE OF GRAVEL SLOPE LANDSLIDE AND EXPERIMENT SIMULATION[J]. Chinese Journal of Rock Mechanics and Engineering, 2002, 21(12): 1831-1834
Authors:Hu Mingjian  Wang Ren  Zhang Pingcang
Abstract:The effect of rainfall on landslide is a widely discussed theme. This paper expatiates the inspiring cause from some aspects such as the substance composition,structure conditions,rainfalls,rainfall density and the stress characteristics etc. We have observed the course inspired by artificial rainfall from the large outdoor landslide experiment. The indoor experiment illuminates that the cohesion and inner friction angle have a chop relationship with the moisture content. The gravel slope landslide is inspired by many factors of which the rainfall is the dominant.
Keywords:rainfall  landslide  moisture content  stress characters  chop
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