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RECOVERY OF ANISOTROPIC SLOPE AFTER THE LANDSLIDE

机译:滑坡后恢复各向异性斜坡

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摘要

The algorithm of finite-element simulation of some sides of effect is adduced. These sides are uneven saturation of grounds with water, not uniform structure of the ground thickness and bounded with this fact the slope anisotropy. The details of reduced anisotropy and its influence on the value of the limit stresses at the places of geometric fractures and at the slide line are given.
机译:提出了影响面有限元模拟的算法。这些侧面是地面的不均匀水饱和度,不是地面厚度的均匀结构,因此以坡度各向异性为界。给出了减小各向异性的细节及其对几何断裂处和滑移线处极限应力值的影响。

著录项

  • 来源
  • 会议地点 Nanjing(CN)
  • 作者

    ZHANG Yi; rnZHANG Rui;

  • 作者单位

    Rysbek Baimakhan@Scientific Center of Fundamental Researches near the Kazakh State Woman's Pedagogical University, Almaty, Kazakhstan--Sarandulam Dashdorj@Hokkaido University, Sapporo, Japan--Nargozy Danaev@Scientific Center of Fundamental Researches near the Kazakh State Woman's Pedagogical University, Almaty, Kazakhstan--Aigerim Baimakhan@Scientific Center of Fundamental Researches near the Kazakh State Woman's Pedagogical University, Almaty, Kazakhstan--Gulnaz Salgaraeva@Scientific Center of Fundamental Researches near the Kazakh State Woman's Pedagogical University, Almaty, Kazakhstan--Gulaym Ylyasova@Scientific Center of Fundamental Researches near the Kazakh State Woman's Pedagogical University, Almaty, Kazakhstan--Nurgul Kurmanbekkizy@Scientific Center of Fundamental Researches near;

  • 会议组织
  • 原文格式 PDF
  • 正文语种
  • 中图分类 灾害地质学;
  • 关键词

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