Prediction of deformation and failure of a large-scale deposit slope during reservoir water level fluctuation
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Prediction of deformation and failure of a large-scale deposit slope during reservoir water level fluctuation
Vol. 32, Issue 6, (2011)
作者机构:
1. 华北水利水电学院 资源与环境学院,郑州,450011
2. 中国科学院地质与地球物理研究所 中国科学院工程地质力学重点实验室,北京,100029
作者简介:
基金信息:
DOI:
CLC:TV223
Online First:21 June 2011,
Published:2011
稿件说明:
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DONG Jin-yu, YANG Ji-hong, SUN Wen-huai, et al. Prediction of deformation and failure of a large-scale deposit slope during reservoir water level fluctuation[J]. 2011, 32(6).
DOI:
DONG Jin-yu, YANG Ji-hong, SUN Wen-huai, et al. Prediction of deformation and failure of a large-scale deposit slope during reservoir water level fluctuation[J]. 2011, 32(6).DOI:
Prediction of deformation and failure of a large-scale deposit slope during reservoir water level fluctuation
Research on deformation and stability of reservoir bank slopes is one of the focus in the world. Taking a deposit slope in the hydropower reservoir area for example
the deformation and failure characteristics of the slope are predicted by FLAC3D while the reservoir level is rising and rapid drawdown. It is indicated that deformation mainly occurred in the deposit body while the reservoir level fluctuating; the deposit body is divided into three regions according to the deformation characteristics: the front traction deformation area with the largest deformation
the middle transition area with the smallest deformation and the posterior passive traction deformation area. Displacement monitoring points are set at different places of the slope body; so the displacement-time graphs during reservoir filling and rapid drawdown of reservoir level are obtained. The monitoring results show that the local instability occurred at the front of the slope during the rapid drawdown of the reservoir level. Owing to the influence of water two potential sliding failure surfaces in slope can be judged based on the shear strain increment.