Analysis of seepage field and stability of clinosol slope under rainfall infiltration

被引:0
作者
Yang, Yixi [1 ]
Guo, Fang [1 ]
机构
[1] Hunan Commun Polytech, Changsha 410132, Hunan, Peoples R China
来源
ADVANCES IN CIVIL AND INDUSTRIAL ENGINEERING, PTS 1-4 | 2013年 / 353-356卷
关键词
slope wash; unsaturated theory; rainfall infiltration; stability;
D O I
10.4028/www.scientific.net/AMM.353-356.307
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
In order to research on slope seepage field and slop stability under rainfall infiltration, this paper combines finite element with limit equilibrium theory to study. The results show that under rainfall, pore water pressure of the slope crest and slope toe in slope wash is greatly influenced by rainfall; Change in the volume moisture content is more sensitive than pore water pressure, volumetric moisture content of each location is increasing quickly at the initial stage of rain, volumetric moisture content in the lower locations is the first to reach saturated due to the continued supply and gravity of the rain; The slope stability reduces with rainfall infiltration, the greater the rainfall intensity, the more obvious decline the slope safety factor.
引用
收藏
页码:307 / 311
页数:5
相关论文
共 6 条
[1]  
[Anonymous], SOIL MECH UNSATURATE
[2]  
Chengdu university of technology national laboratory of geological hazard prevention and geological environmental protection, 2004, RAINF IND LANDSL RES
[3]  
FREDLUND D G, 1997, UNSATURATED SOIL MEC
[4]   Experimental investigations of the soil-water characteristics of a volcanic soil [J].
Ng, CWW ;
Pang, YW .
CANADIAN GEOTECHNICAL JOURNAL, 2000, 37 (06) :1252-1264
[5]   A CLOSED-FORM EQUATION FOR PREDICTING THE HYDRAULIC CONDUCTIVITY OF UNSATURATED SOILS [J].
VANGENUCHTEN, MT .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1980, 44 (05) :892-898
[6]  
Xu Yongfu, 1999, UNSATURATED SOIL STR