Coupled analysis of fracture rock mass slope saturated-unsaturated seepage field and stress field in flood discharge atomized rain area
|更新时间:2026-06-25
|
Coupled analysis of fracture rock mass slope saturated-unsaturated seepage field and stress field in flood discharge atomized rain area
Vol. 29, Issue 9, (2008)
作者机构:
1. 河海大学 交通学院,南京,210098
2. 河海大学 岩土工程研究所,南京,210098
作者简介:
基金信息:
DOI:
CLC:O357
Online First:03 August 2013,
Published:2008
稿件说明:
移动端阅览
WANG Huan-ling XU Wei-ya TONG Fu-guo. Coupled analysis of fracture rock mass slope saturated-unsaturated seepage field and stress field in flood discharge atomized rain area[J]. 2008, 29(9).
DOI:
WANG Huan-ling XU Wei-ya TONG Fu-guo. Coupled analysis of fracture rock mass slope saturated-unsaturated seepage field and stress field in flood discharge atomized rain area[J]. 2008, 29(9).DOI:
Coupled analysis of fracture rock mass slope saturated-unsaturated seepage field and stress field in flood discharge atomized rain area
Flood discharge atomized rain is the non-neglectable activator for rock mass landslide
which besides the rainfall. At first
through the relation between seepage characters of fracture rock mass and stress
elastic-plastic constitutive equation of fracture rock mass and control equation of seepage field
the equation continue media model of seepage and stress field coupling is established. Secondly
a 3-D finite element program of saturated-unsaturated seepage and stress coupling under atomized rain programmed
the two-field coupling is solved by iteration method. Finally
taking a typical project for example
the geological model is established according to the earth’s surface information
excavation information
terrane borderline information
drainage hole and purdah information; the rock mass deformation
stress and plastic area are analyzed in detail by coupling computation
the analysis shows that the slope stability has closely related with the change of saturated-unsaturated seepage field of rock mass system; the seepage field of rock mass system must be considered when estimating slope stability. The result can provide some scientific foundation for project slope stability estimation.