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A three-dimensional mesoscale model for progressive time-dependent deformation and fracturing of brittle rock with application to slope stability

机译:一种三维Messcale模型,用于剥削稳定性的脆性时间依赖变形和脆性岩体的压裂

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摘要

An understanding of progressive time-dependent deformation is essential for determining appropriate measures to ensure the long-term integrity of rock-masses surrounding engineering structures. We propose a 3D numerical model, that uses the Norton-Bailey creep law and a time-independent damage evolution law, to investigate the progressive time-dependent deformation and fracturing of brittle rock. The model considers material heterogeneity and the concept of mesoscopic renormalization at the mesoscale. The cooperative interaction between microcrack distribution and damage evolution leads to local material degeneration as a function of increasing time in the model. First, the input parameters for the model were calibrated and the model was validated using laboratory experiments. Numerical creep simulations were then performed for a range of constant stresses. Our model can accurately replicate the evolution of strain and strain rate as a function of time, the output of acoustic emission energy, and the emergence of a macroscopic failure plane seen in laboratory experiments. Our simulations also show that the minimum creep strain rate and the time-to-failure increase and decrease, respectively, as stress is increased, also seen in laboratory experiments. For example, increasing the differential stress by 10 MPa increased the minimum creep strain rate increased by an order of magnitude. Finally, we use the proposed 3D model to investigate the time-dependent stability of an engineering-scale rock slope containing faults at the Fushun West Open Pit coal mine. A small increase in fault-adjacent damage was observed after 40 days and, between 60 and 120 days, the damage on the side of the slope increased. After 140 days, the localized growth of the damaged elements split the slope into two segments, resulting in slope failure. Our 3D numerical model highlights potential slope instability in the Fushun West Open Pit coal mine and can be used to investigate slope stability in engineering projects worldwide.
机译:对进步时间依赖变形的理解对于确定适当的措施来确保围绕工程结构的岩体长期完整性是必不可少的。我们提出了一种使用Norton-Bailey蠕变法和一个无关的损伤进化法的3D数值模型,以研究脆性岩石的逐步时间依赖性变形和压裂。该模型考虑了Mesoscale在Mesoscale中的材料异质性和介观重整化的概念。微裂纹分布与损伤进化之间的合作相互作用导致局部材料变性,作为模型中提高时间的函数。首先,校准模型的输入参数,使用实验室实验验证模型。然后对一系列恒定应力进行数值蠕变模拟。我们的模型可以用作时间,声发射能量的输出,以及在实验室实验中看到的宏观失效平面的出现来准确地复制应变和应变率的演变。我们的仿真还表明,在实验室实验中也可以分别在压力增加时,最小蠕变应变速率和失效时间增加和减少。例如,增加差分应力10MPa增加,增加最小蠕变应变速率增加了幅度。最后,我们使用所提出的3D模型来调查抚顺西露煤矿的工程规模岩石坡的时间依赖稳定性。在40天后观察到故障相邻损坏的小幅增加,在60至120天之间,斜率侧的损坏增加。 140天后,损坏元素的局部生长将斜率分成两个段,导致斜率衰竭。我们的3D数值模型突出了抚顺西露煤矿的潜在坡不稳定性,可用于调查全球工程项目的坡度稳定性。

著录项

  • 来源
    《Computers and Geotechnics》 |2021年第7期|104160.1-104160.15|共15页
  • 作者单位

    Northeastern Univ Ctr Rock Instabil & Seism Res Shenyang 110819 Peoples R China;

    Northeastern Univ Ctr Rock Instabil & Seism Res Shenyang 110819 Peoples R China;

    Univ Strasbourg CNRS UMR 7063 Inst Terre & Environm Strasbourg 5 Rue Rene Descartes F-67084 Strasbourg France;

    UCL Dept Earth Sci Rock & Ice Phys Lab Gower St London WC1E 6BT England;

    Northeastern Univ Ctr Rock Instabil & Seism Res Shenyang 110819 Peoples R China;

    Shandong Univ Sci & Technol Coll Energy & Min Engn Qingdao 266590 Shandong Peoples R China;

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

    3D model; Time-dependent deformation; Creep; Relaxation; Rock slope;

    机译:3D模型;时间依赖变形;蠕变;放松;摇滚斜坡;

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