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A numerical analysis of rock creep-induced slide: a case study from Jiweishan Mountain, China

机译:岩石蠕变滑坡的数值分析:以中国鸡尾山为例

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摘要

Landslides and slope failures are very common phenomena in hilly regions, Southwestern China. These are hazardous because of the accompanying progressive movement of the slope-forming-material. To minimize the landslide effects, slope failure analysis and stabilization require in-depth understanding of the process that governs the behavior of the slope. The present paper first briefly describes a three-dimensional numerical brittle creep model for rock. The model accounts for material heterogeneity, through a stochastic local failure stress field, and local material degradation using an exponential material softening law. Then a case study of the Jiweishan rockslide that occurred in China is numerically investigated considering the effect of the mining activity. Numerical simulations visualize the entire process of the Jiweishan rockslide from the fracture initiation, propagation and coalescence. The distribution and evolution of associated stress and deformation field during the slide are also presented. Numerical simulations show that the underground mining excavations have remarkably negative effect on the stability of the rock slope, which is one of the important triggering factors of the rockslide. Moreover, it is possible to take some precautions for the unstable failure of rock mass by monitoring acoustic emission (AE) events or mi-croseismicities since the occurrence of clusters of AE events prior to the final unstable rockslide. The results are of general interest, because they can be applied to the investigation of time-dependent instability in rock masses, to the mitigation of associated rock hazards in rock engineering, and even to a better understanding of the seismic activities in geological and geophysical phenomena occurring in the earth's crust.
机译:滑坡和边坡破坏是中国西南丘陵地区非常普遍的现象。这些是危险的,因为伴随有斜坡形成材料的逐渐运动。为了最大程度地减少滑坡的影响,边坡破坏分析和稳定需要深入了解控制边坡行为的过程。本文首先简要描述了岩石的三维数值脆性蠕变模型。该模型通过随机的局部破坏应力场解释材料的异质性,并使用指数材料软化定律解释材料的局部降解。然后,考虑采矿活动的影响,对中国发生的鸡尾山滑坡进行了案例研究。数值模拟从裂隙的起裂,扩展和合并可视化了吉尾山滑坡的整个过程。还介绍了滑动过程中相关应力和变形场的分布和演变。数值模拟表明,地下采矿对岩质边坡的稳定性有明显的负面影响,这是引起岩层滑坡的重要触发因素之一。此外,由于在最终的不稳定岩石滑坡之前发生了AE事件簇,因此可以通过监测声发射(AE)事件或微顺震性来预防岩体的不稳定破坏。这些结果具有普遍意义,因为它们可用于研究岩体中随时间变化的不稳定性,减轻岩石工程中相关的岩石危害,甚至可以更好地理解地质和地球物理现象中的地震活动。发生在地壳中。

著录项

  • 来源
    《Environmental earth sciences》 |2014年第6期|2111-2128|共18页
  • 作者单位

    Center for Rock Instability and Seismicity Research, Northeastern University, Shenyang 110819, China;

    State Key Laboratory of Geo-hazard Prevention and Geo-environment Protection, Chengdu University of Technology, Chengdu 610059, China;

    State Key Laboratory of Geo-hazard Prevention and Geo-environment Protection, Chengdu University of Technology, Chengdu 610059, China;

    School of Civil Engineering, Dalian University of Technology, Dalian 116024, China;

    Center for Rock Instability and Seismicity Research, Northeastern University, Shenyang 110819, China;

    School of Civil Engineering, Dalian University of Technology, Dalian 116024, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Time-dependent behavior; Rock creep; Numerical simulation; Rockslide;

    机译:时间依赖性行为;岩石蠕变;数值模拟岩滑;

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