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Numerical investigation into the blasting-induced damage characteristics of rocks considering the role of in-situ stresses and discontinuity persistence

机译:考虑地应力和不连续性作用的岩石爆破损伤特征数值研究

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This paper presents a 3D coupled Smoothed Particle Hydrodynamics (SPH) and Finite Element Method (FEM) model, which was developed to investigate the extent of damage zone and fracture patterns in rock due to blasting. The RHT material model was used to simulate the blasting-induced damage in rock. The effects of discontinuity persistence and high in-situ stresses on the evolution of blasting-induced damage were investigated. Results of this study indicate that discontinuity persistence and spatial distribution of rock bridges have a significant influence on the evolution of blasting-induced damage. Furthermore, high in-situ stresses also have a significant influence on the propagation of blasting-induced fractures, as well as the patterns of fracture networks. It is also shown that the blasting-induced cracks are often induced along the direction of the applied high initial stresses. Moreover, additional cracks are normally generated at the edges of the rock bridges probably due to the relatively high stress concentration.
机译:本文提出了一种3D耦合的平滑粒子流体动力学(SPH)和有限元方法(FEM)模型,用于研究爆破造成的岩石破坏区域和裂缝模式的程度。 RHT材料模型用于模拟岩石中爆破引起的破坏。研究了不连续性持久性和高地应力对爆破损伤演变的影响。这项研究的结果表明,岩石桥梁的不连续性持久性和空间分布对爆破损伤的演变有重大影响。此外,高地应力也对爆破引起的裂缝的扩展以及裂缝网络的模式产生重大影响。还表明,爆破引起的裂纹通常是沿着施加的高初始应力的方向诱发的。此外,可能由于相对较高的应力集中,在岩石桥梁的边缘通常会产生其他裂纹。

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