Unsaturated seepage analysis of the influence of water level fluctuation on pore water pressure of landslide in reservoir area
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Unsaturated seepage analysis of the influence of water level fluctuation on pore water pressure of landslide in reservoir area
Vol. 29, Issue S1, (2008)
作者机构:
1. 中南大学 信息物理工程学院,长沙,410083
2. 中南大学 资源与安全工程学院,长沙,410083
3. 中国水电工程顾问集团公司中南勘测设计研究院,长沙,410014
作者简介:
基金信息:
DOI:
CLC:TU457
Online First:15 April 2016,
Published:2008
稿件说明:
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LIU Qun-yi, ZHU Zi-qiang, HE Xian-qi, et al. Unsaturated seepage analysis of the influence of water level fluctuation on pore water pressure of landslide in reservoir area[J]. 2008, 29(S1).
DOI:
LIU Qun-yi, ZHU Zi-qiang, HE Xian-qi, et al. Unsaturated seepage analysis of the influence of water level fluctuation on pore water pressure of landslide in reservoir area[J]. 2008, 29(S1).DOI:
Unsaturated seepage analysis of the influence of water level fluctuation on pore water pressure of landslide in reservoir area
Iandslide in a certain reservoir area is chosen as the engineering background. According to the saturated-unsaturated seepage equation
the dynamic response of pore water pressure in the landslide influenced by the fluctuation of water level is studied when considering the infiltration characteristics and the fluctuation velocity of water level. The analysis results show that (1) when the water level fluctuates
the saturated permeability coefficient has great impact on the initial water level under the same infiltration condition; with the increase of the saturated permeability coefficient
the water level becomes lower
and the water level line becomes more smooth
which has smaller impact on the dynamic and static pore water pressure
and is good to the slope stability; (2) with the increase of fluctuation velocity of water level
the response of water level lags behind
the water level line becomes steeper
which causes greater dynamic pore water pressure to the slope