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Development of a fault-rupture environment in 3D: A numerical tool for examining the mechanical impact of a fault on underground excavations

机译:3D断层破裂环境的开发:一种用于检查断层对地下基坑的机械影响的数值工具

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摘要

While faults are commonly simulated as a single planar or non-planar interface for a safety or stability analysis in underground mining excavation, the real 3D structure of a fault is often very complex, with different branches that reactivate at different times. Furthermore, these branches are zones of nonzero thickness where material continuously undergoes damage even during interseismic periods. In this study, the initiation and the initial evolution of a strike-slip fault was modeled using the FLAC3D software program. The initial and boundary conditions are simplified, and mimic the Riedel shear experiment and the constitutive model in the literature. The FLAC3D model successfully replicates and creates the 3D fault zone as a strike-slip type structure in the entire thickness of the model. The strike-slip fault structure and normal displacement result in the formation of valleys in the model. Three panels of a longwall excavation are virtually placed and excavated beneath a main valley. The characteristics of stored and dissipated energy associated with the panel excavations are examined and observed at different stages of shear strain in the fault to evaluate bump potential. Depending on the shear strain in the fault, the energy characteristics adjacent to the longwall panels present different degrees of bump potential, which is not possible to capture by conventional fault simulation using an interface.
机译:虽然通常将故障模拟为单个平面或非平面接口,以进行地下采矿开挖的安全性或稳定性分析,但故障的真实3D结构通常非常复杂,具有在不同时间重新激活的不同分支。此外,这些分支是厚度不为零的区域,即使在地震期间,材料也不断遭受破坏。在这项研究中,使用FLAC3D软件程序对走滑断层的起步和初始演化进行了建模。简化了初始条件和边界条件,并模仿了Riedel剪切实验和本构模型。 FLAC3D模型成功复制并在模型的整个厚度中创建了3D断层带,作为走滑型结构。走滑断层的构造和法向位移导致了模型中谷的形成。长墙开挖的三块面板实际上放置在主山谷下方,并在其下方开挖。在断层的剪切应变的不同阶段,检查和观察与面板开挖有关的存储和耗散能量的特征,以评估碰撞电位。根据断层中的剪切应变,与长壁板相邻的能量特性会呈现不同程度的碰撞电位,这无法通过使用接口的常规断层模拟来捕获。

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