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库水位下降的饱和-非饱和土坝渗流数值模拟

Numerical simulation of saturated-unsturated earth dam during descent of reservoir water level

中文摘要英文摘要

基于非饱和土渗流的理论,借助Geo-slope的有限元数值模拟软件,对库水位下降过程中的饱和-非饱和土坝进行了数值模拟分析,分析结果给出了坝体在库水位下降的过程中,坝体中孔隙水压力的消散状况以及坝体中自由水面位置、形态的变化情况等。与将坝体视为完全饱和状况下分析结果进行对比发现:自由水面在库水位下降的各个时刻,两者计算得出的自由水面的位置、形态均存在较大的差异,并且,两者计算得出的坝体稳定系数也存在差异,库水位降低的过程中,前者的稳定系数要低;库水位稳定一年后,前者的稳定性会高于后者。

Based on the theory of seepage in unsaturated soil, the infinite numerical simulation software named Geo-slope was adopted, to simulate the earth dam during the descent of reservoir water level. The analysis results were obtained, including the pore water pressure, the position and configuration of seepage line, etc. Compared with the results calculated under saturated state, difference such as the height and the configuration of seepage line existed between each other, also, the stability factor calculated of each other were not the same, the former was lower than the later during the descent of reservoir water level, but the later was lower than the former when the reservoir water level achieved stability for one year.

李新军、夏元友、徐杨军

水利枢纽、水工建筑物

非饱和土非稳定渗流数值模拟自由水面

unsaturated soiltransient-seepagenumerical simulationseepage line

李新军,夏元友,徐杨军.库水位下降的饱和-非饱和土坝渗流数值模拟[EB/OL].(2010-04-22)[2025-08-23].http://www.paper.edu.cn/releasepaper/content/201004-841.点此复制

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