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李靖, 周欣华, 党进谦. 黄土边坡稳定性图解法[J]. 岩土工程学报, 1998, 20(4): 43-46.
引用本文: 李靖, 周欣华, 党进谦. 黄土边坡稳定性图解法[J]. 岩土工程学报, 1998, 20(4): 43-46.
Li Jing, Zhou Xinhua, Dang Jinqian. Graphic method for the stability of loess slopes[J]. Chinese Journal of Geotechnical Engineering, 1998, 20(4): 43-46.
Citation: Li Jing, Zhou Xinhua, Dang Jinqian. Graphic method for the stability of loess slopes[J]. Chinese Journal of Geotechnical Engineering, 1998, 20(4): 43-46.

黄土边坡稳定性图解法

Graphic method for the stability of loess slopes

  • 摘要: 针对边坡稳定分析计算方法冗长繁琐、计算量大以及已有图表解法仍需试算等不足,考虑到影响黄土边坡稳定的主要因素,如岩性、地形、地下水条件、坡体含水量以及地震烈度等,采用简化毕晓普法并归化其计算式为无因次方程,借助计算机及边坡稳定分析程序,获得了简捷明快、使用方便的稳定分析图。同时,在大量系统计算的基础上,分析了地震烈度、强度指标、孔隙水压力系数等参数对危险滑面及稳定曲线位置的影响。结果表明,滑坡范围随地震烈度、孔隙水压力、粘聚力的增大而增大,随土体内摩擦角的增大而减小。

     

    Abstract: In view of the disadvantages of complicated calculation process for the current methods of stability analysis of earth slopes,a simple and convenient graphical method is established, taking many main factors into consideration, such as rock characteristics , topography, underground water condition, water content of soil and earthquake intensity etc. The simplified Bishop′s method is used to induce a dimensionless equation, and a concise graph is obtained by systematic calculation using relevant computer programs. Also, the effect of earthquake intensity, strength parameters, coefficient of pore pressure and other parameters are analyzed. The result show that, the slide area extends with the increase of earthquake intensity, pore pressure , cohesion of soil , whill it decreases with the increase of angle of internal friction φ .

     

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