郭建军, 王俊杰, 黎洪光, 闵志华. 2017: 坡后土体推力作用下反倾节理岩质边坡次生倾倒机理分析. 工程地质学报, 25(5): 1205-1212. DOI: 10.13544/j.cnki.jeg.2017.05.004
    引用本文: 郭建军, 王俊杰, 黎洪光, 闵志华. 2017: 坡后土体推力作用下反倾节理岩质边坡次生倾倒机理分析. 工程地质学报, 25(5): 1205-1212. DOI: 10.13544/j.cnki.jeg.2017.05.004
    GUO Jianjun, WANG Junjie, LI Hongguang, MIN Zhihua. 2017: ANALYSIS OF SECONDARY TOPPLING MECHANISM OF JOINTED ROCK SLOPE UNDER SOIL PRESSURE. JOURNAL OF ENGINEERING GEOLOGY, 25(5): 1205-1212. DOI: 10.13544/j.cnki.jeg.2017.05.004
    Citation: GUO Jianjun, WANG Junjie, LI Hongguang, MIN Zhihua. 2017: ANALYSIS OF SECONDARY TOPPLING MECHANISM OF JOINTED ROCK SLOPE UNDER SOIL PRESSURE. JOURNAL OF ENGINEERING GEOLOGY, 25(5): 1205-1212. DOI: 10.13544/j.cnki.jeg.2017.05.004

    坡后土体推力作用下反倾节理岩质边坡次生倾倒机理分析

    ANALYSIS OF SECONDARY TOPPLING MECHANISM OF JOINTED ROCK SLOPE UNDER SOIL PRESSURE

    • 摘要: 次生倾倒破坏是层状反倾岩质边坡的一种主要破坏模式,极限平衡理论是分析倾倒破坏的常用方法,研究反倾节理岩质边坡次生倾倒破坏机理对边坡工程众多的西南山区基础设施建设具有重要的工程指导意义。在Goodman和Bray块体倾倒破坏极限平衡分析方法的基础上,建立了考虑地下水压力、节理连通率、岩体黏聚力等影响因素的反倾岩质边坡在坡后土体推力作用下的次生倾倒地质力学模型,提出了坡后土体推力作用下的反倾节理岩质边坡次生倾倒破坏的解析分析方法,推导出了边坡各岩层下推力的解析表达式,提出了边坡倾倒破坏的综合安全系数,并编写了对应的matlab计算程序,为该类边坡的设计和加固提供了理论依据。通过算例分析表明,与单纯岩质边坡块体倾倒破坏相比,该类边坡次生倾倒破坏形式的特点是破坏基准面以上岩层自上而下依次分为滑移区、倾倒区和稳定区3个部分;地下水压力、节理连通率、底裂面岩体黏聚力对各岩层的破坏形式、稳定安全系数大小都具有明显影响,尤其是在坡体中下部及坡脚部分最为敏感;而各岩层稳定安全系数最小的区域集中于边坡中上部。

       

      Abstract: Secondary toppling failure is one of typical instabilities of steep stratified rock slopes. The limit equilibrium analysis method is the main method to analyze the toppling failure of rock slopes. Analysis of secondary toppling failure of counter-tilt jointed rock slopes has an important bearing on engineering practice, especially for mountain area of southwest China where there are many slope engineering. Based on the analysis method of limit equilibrium proposed by Goodman and Bray, a geomechanical model of the secondary toppling of counter-tilt jointed rock slope under the action from rear soil pressure are developed, The related analysis method is proposed. This model takes into account the factors such as groundwater pressure, joint connectivity, and rock cohesion. A formulation is derived for calculating the pushing force of each rock formation. The comprehensive safety coefficient is given. The stability of secondary toppling of counter-tilt jointed rock slope can be easily analyzed using a Matlab program, which provides a theoretical basis for the design and reinforce of this type of slope. An example is introduced. It analyses the influence of groundwater pressure, joint connectivity as well as rock cohesion on the pushing force of each rock formation and comprehensive safety coefficient. Compared with the block toppling failure of rock slopes, for secondary toppling failure of counter-tilt jointed rock slopes, from top to bottom, the rock formation above destruction surface is divided into three parts:the slip zone, the toppling area and the stabilization zone. The groundwater pressure, joint connectivity and the rock cohesion of the underlying fractured rock have obvious influence on the failure form and stability safety coefficient of each rock formation, especially in the lower part of the slope and the foot part of the slope. The minimum stability factor of each rock formation is concentrated in the upper part of the slope.

       

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