Numerical study on rainfall infiltration in rock-soil slop

P5; A mathematical model for the rain infiltration in the rock-soil slop has been established and solved by using the finite element method. The unsteady water infiltrating process has been simulated to get water content both in the homogeneous and heterogeneous media. The simulated results show tha...

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Published in中国科学E辑(英文版) Vol. 48; no. z1; pp. 33 - 46
Main Authors LIU Yuewu, LIU Qingquan, CHEN Huixin, GONG Xin, ZHANG Dawei, YAO Deliang, LI Lianxiang
Format Journal Article
LanguageEnglish
Published Division of Engineering Science, Institute of Mechanics, Chinese Academy of Sciences, Beijing 100080, China 2005
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Abstract P5; A mathematical model for the rain infiltration in the rock-soil slop has been established and solved by using the finite element method. The unsteady water infiltrating process has been simulated to get water content both in the homogeneous and heterogeneous media. The simulated results show that the rock blocks in the rock-soil slop can cause the wetting front moving fast. If the rain intensity is increased, the saturated region will be formed quickly while other conditions are the same. If the rain intensity keeps a constant, it is possible to accelerate the generation of the saturated region by properly increasing the vertical filtration rate of the rock-soil slop. However, if the vertical filtration rate is so far greater than the rain intensity, it will be difficult to form the saturated region in the rock-soil slop. The numerical method was verified by comparing the calculation results with the field test data.
AbstractList P5; A mathematical model for the rain infiltration in the rock-soil slop has been established and solved by using the finite element method. The unsteady water infiltrating process has been simulated to get water content both in the homogeneous and heterogeneous media. The simulated results show that the rock blocks in the rock-soil slop can cause the wetting front moving fast. If the rain intensity is increased, the saturated region will be formed quickly while other conditions are the same. If the rain intensity keeps a constant, it is possible to accelerate the generation of the saturated region by properly increasing the vertical filtration rate of the rock-soil slop. However, if the vertical filtration rate is so far greater than the rain intensity, it will be difficult to form the saturated region in the rock-soil slop. The numerical method was verified by comparing the calculation results with the field test data.
Author LI Lianxiang
YAO Deliang
CHEN Huixin
ZHANG Dawei
GONG Xin
LIU Qingquan
LIU Yuewu
AuthorAffiliation Division of Engineering Science, Institute of Mechanics, Chinese Academy of Sciences, Beijing 100080, China
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  fullname: YAO Deliang
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  fullname: LI Lianxiang
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rock-soil block
water content
Finite Element Method (FEM)
infiltration
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