长江科学院院报 ›› 2016, Vol. 33 ›› Issue (6): 99-104.DOI: 10.11988/ckyyb.20150169

• 岩土工程 • 上一篇    下一篇

复合型滑坡推力计算方法研究

谭福林,胡新丽,张玉明,方堃,李蕊   

  1. 中国地质大学武汉 工程学院,武汉 430074
  • 收稿日期:2015-03-10 出版日期:2016-05-25 发布日期:2016-06-12
  • 作者简介:谭福林(1990-),男,江西赣州人,硕士研究生,主要从事岩土体稳定性评价与模型实验研究工作,(电话)18064077915 (电子信箱)tanfulin868889@163.com。    通讯作者:胡新丽(1968-),女,河南许昌人,教授,博士生导师,主要从事岩土工程稳定性评价、地质灾害防治科研设计及教学工作,(电话)13907152610(电子信箱)huxinli@cug.edu.cm。
  • 基金资助:
    国家重点基础研究发展计划“973”项目(2011CB710604);国家自然科学基金项目(41272305)

A Method of Calculating the Thrust of Complex Landslide

TAN Fu-lin, HU Xin-li, ZHANG Yu-ming, FANG Kun, LI Rui   

  1. Faculty of Engineering, China University of Geosciences, Wuhan 430074, China
  • Received:2015-03-10 Online:2016-05-25 Published:2016-06-12

摘要: 复合型滑坡是推移式和牵引式的组合,既有牵引式滑坡的特点又有推移式滑坡的性质,通过对复合型滑坡形成机理的研究,揭示了复合型滑坡具有前部牵引—后部加载—中部滑带剪断贯通—最终整体滑移失稳的变形破坏模式,对应地将复合型滑坡分为3个区前缘启动区(牵引作用)、中间主滑区、后缘启动区(加载作用)。针对不同区的破坏形式和受力特点,以及不同区之间的相互作用过程,建立了准确合理的地质力学计算模型,对不同区推力进行详细的计算推导。在推力计算过程中,复合型滑坡推力计算具有区段针对性,前缘启动区和后缘启动区需要考虑与中间主滑区之间的相互作用,而中间主滑区的稳定性是对整个滑坡起主导作用,在计算推力时,既要考虑前缘启动区阻滑段的缺失又要考虑后缘启动区的加载效应。以典型复合型滑坡为例,通过计算充分说明此推力计算方法的合理性,为复合型滑坡防治工程设计提供计算方法。

关键词: 复合型滑坡, 变形破坏模式, 地质力学计算模型, 推力计算, 条块受力分析

Abstract: Complex landslide is the combination of load-caused landslide and retrogressive landslide, with the characteristics of both load-caused landslide and retrogressive landslide. Through research on the formation mechanism of complex landslide, we reveal that complex landslide successively experiences the failure modes of retrogression in the front side, load in the backside, penetration of slip zone in the middle, and finally global sliding instability. Correspondingly, we divide complex landslide into three zones start area in the leading edge (tractive effect), main slide area in the middle, and start area in the trailing edge (loading effect). According to the failure modes and mechanical characteristics of different areas, as well as the interaction among these areas, we establish a calculation model of geomechanics, and derive the thrust of the three areas in detail. The thrust calculation for different areas should be specific. For the calculation of leading edge start area and trailing edge start area, their interactions with the main sliding area should be considered. And the stability of the main sliding area plays a dominant role in the whole landslide. It is necessary to consider the absence of slide-resistance of the leading edge start area and also the loading effect of the trailing edge start area. Calculation example of a typical complex landslide proves the rationality of the thrust calculation method. This research provides a reference for the prevention and control of complex landslide.

Key words: complex landslide, deformation and failure mode, geomechanical model, calculation of thrust, stress analysis of slices and blocks

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