赵伟华, 黄润秋, 赵建军, 巨能攀, 李果. 2011: 强震条件下碎裂岩体崩塌机理及崩塌后壁对堆积体稳定性影响研究. 工程地质学报, 19(2): 205-212.
    引用本文: 赵伟华, 黄润秋, 赵建军, 巨能攀, 李果. 2011: 强震条件下碎裂岩体崩塌机理及崩塌后壁对堆积体稳定性影响研究. 工程地质学报, 19(2): 205-212.
    ZHAO Weihua, HUANG Runqiu, ZHAO Jianjun, JU Nengpan, Li Guo. 2011: ROCKFALL MECHANISM OF CATACLASTIC ROCK MASS AND INFLUENCE OF BACK WALL UPON THE STABILITY OF ACCUMULATION UNDER STRONG EARTHQUAKE. JOURNAL OF ENGINEERING GEOLOGY, 19(2): 205-212.
    Citation: ZHAO Weihua, HUANG Runqiu, ZHAO Jianjun, JU Nengpan, Li Guo. 2011: ROCKFALL MECHANISM OF CATACLASTIC ROCK MASS AND INFLUENCE OF BACK WALL UPON THE STABILITY OF ACCUMULATION UNDER STRONG EARTHQUAKE. JOURNAL OF ENGINEERING GEOLOGY, 19(2): 205-212.

    强震条件下碎裂岩体崩塌机理及崩塌后壁对堆积体稳定性影响研究

    ROCKFALL MECHANISM OF CATACLASTIC ROCK MASS AND INFLUENCE OF BACK WALL UPON THE STABILITY OF ACCUMULATION UNDER STRONG EARTHQUAKE

    • 摘要: 5 12 汶川地震的强震作用诱发产生了大量崩塌地质灾害,且多发生于碎裂结构岩体中。崩塌后斜坡后缘岩体及前缘堆积体的稳定性和后缘岩体对前缘堆积体稳定性的影响研究同样是震后灾害所面临的问题。以干河沟沟口斜坡为例,在分析该斜坡结构特征及崩塌机理的基础上,采用二维离散元软件UDEC模拟了斜坡在天然或强震条件下的稳定状态和可能失稳过程; 运用极限平衡法对陡壁岩体再次崩塌,产生新物质堆载在现有崩塌堆积体后缘前、后分别建立模型进行了稳定性分析。研究结果表明:碎裂岩体崩塌过程可分为应力重分布、潜在崩塌体形成和地震诱发崩塌3个阶段。崩塌堆积体在考虑后缘堆载作用之前,在天然或地震环境下均处于相对稳定状态,考虑堆载作用之后,其可能会在地震条件下失稳。离散元法和极限平衡法的组合使用,对于解决同类斜坡的同类问题切实可行。

       

      Abstract: The Wenchuan 8.0 earthquake triggered a huge number of rockfall hazards. The hazards most happened in cataclastic rock mass. The respective stability of the back wall and the front accumulation of the slope and the influence of the back wall upon the stability of accumulation are problems that are faced by people after the earthquake. This paper takes the Ganhekou rockfalling accumulation as a example. It is based on analysis of the structure feature and genetic mechanism of the slope. It uses the 2D Discrete Element MethodUDEC to simulate the stability status and possible failure process of the slope under nature or earthquake condition.It uses the limit equilibrium theory based models and analyse the stability of accumulation before or after loaded by new substance generated by new rockfall. The results show that the genetic process of rockfalling accumulation can divided to stress redistribution, the formation of potential rockfall mass and rockfall induced by earthquake three phases. Before loading function, the accumulation is relatively stable both under nature or earthquake condition. But after considering the function of loading, it may fail under earthquake. The combined use of discrete element method and limit equilibrium method are practicable way for solving similar problem of similar slopes.

       

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