岩土工程
孔隙水压力
极限分析
阿太堡极限
土壤水分
极限(数学)
地质学
环境科学
土壤科学
工程类
含水量
结构工程
有限元法
数学
数学分析
作者
J. Kim,Rodrigo Salgado,Hai-Sui Yu
出处
期刊:Journal of Geotechnical and Geoenvironmental Engineering
[American Society of Civil Engineers]
日期:1999-01-01
卷期号:125 (1): 49-58
被引量:95
标识
DOI:10.1061/(asce)1090-0241(1999)125:1(49)
摘要
The limit-equilibrium method is commonly used for slope stability analysis. However, it is well-known that the solution obtained from the limit-equilibrium method is not rigorous, because neither static nor kinematic admissibility conditions are satisfied. Limit analysis takes advantage of the lower- and upper-bound theorems of plasticity to provide relatively simple but rigorous bounds on the true solution. In this paper, three-noded linear triangular finite elements are used to construct both statically admissible stress fields for lower-bound analysis and kinematically admissible velocity fields for upper-bound analysis. By assuming linear variation of nodal and elemental variables, the determination of the best lower- and upper-bound solution may be set up as a linear programming problem with constraints based on the satisfaction of static and kinematic admissibility. The effects of pore-water pressure are considered and incorporated into the finite-element formulations so that effective stress analysis of saturated slopes may be done. Results obtained form limit analysis of simple slopes with different ground-water patterns are compared with those obtained from the limit-equilibrium method.
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