马凤山, 丁阔, 赵海军, 郭捷, 卢蓉. 2018: 金属矿开采节理演化诱发覆岩变形失稳机制研究. 工程地质学报, 26(1): 145-156. DOI: 10.13544/j.cnki.jeg.2018.01.016
    引用本文: 马凤山, 丁阔, 赵海军, 郭捷, 卢蓉. 2018: 金属矿开采节理演化诱发覆岩变形失稳机制研究. 工程地质学报, 26(1): 145-156. DOI: 10.13544/j.cnki.jeg.2018.01.016
    MA Fengshan, DING Kuo, ZHAO Haijun, GUO Jie, LU Rong. 2018: FAILURE MECHANISM OF OVERLYING ROCK DEFORMATION INDUCED BY JOINTS DEVELOPMENT IN METAL MINE. JOURNAL OF ENGINEERING GEOLOGY, 26(1): 145-156. DOI: 10.13544/j.cnki.jeg.2018.01.016
    Citation: MA Fengshan, DING Kuo, ZHAO Haijun, GUO Jie, LU Rong. 2018: FAILURE MECHANISM OF OVERLYING ROCK DEFORMATION INDUCED BY JOINTS DEVELOPMENT IN METAL MINE. JOURNAL OF ENGINEERING GEOLOGY, 26(1): 145-156. DOI: 10.13544/j.cnki.jeg.2018.01.016

    金属矿开采节理演化诱发覆岩变形失稳机制研究

    FAILURE MECHANISM OF OVERLYING ROCK DEFORMATION INDUCED BY JOINTS DEVELOPMENT IN METAL MINE

    • 摘要: 金属矿开采诱发覆岩变形是一个复杂的力学问题,在工程活动的扰动下,采空区围岩的原始应力状态将被打破,引起覆岩的应力重分布,从而达到新的应力平衡状态。当覆岩中存在一些软弱结构面时,这些软弱结构面将不断地发展、演化,并可能出现贯通,其对覆岩的变形和破坏具有明显的影响。针对节理条件这一变量,采用Udec二维离散元模型,分析了双岩桥模型和四岩桥模型中各岩桥破裂特征及机制,并对比了两组模型中顶板应力释放规律及特点。采用3组对比模型实验,分析了0°/90°,45°/45°,20°/70°节理条件下岩移特点及变形机制。基于数值模型,对镜儿泉矿区实际节理条件下的地表变形特征和沉陷范围进行了研究,模型结果与地表变形GPS监测结果具有很好的一致性。

       

      Abstract: The overlying rock mass deformation induced by mining is complex mechanical issue in metal mine because of its complicated conditions. Mining operations could change original stresses distribution of surrounding rock, that lead to stresses redistribution of overlying rock then reach a new balance. Structural planes have some influence on overlying rock deformation and failure when they developed and connected. for this situation, we built a 2-dimension discrete element method model utilized in Udec, and analyzed break characteristics and mechanisms of 2-rock-bridge and 4-rock-bridge. We also conducted some comparative studies of stress relief regulation in roof rock. We chose three experimental groups, which joint conditions are 0°/90°, 45°/45°, 20°/70°respectively, to analyze deformation mechanism of rock mass movement. by numerical simulation experiment, we demonstrated the ground movement characteristic and subsidence region. the experimental results have consistency with monitoring data of surface subsidence by GPS.

       

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