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Simulation of crack propagation in rocks by XFEM

机译:XFEM岩石裂纹繁殖的仿真

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Understanding the failure mode and crack propagation in rock can provide useful information for safe and economic design of various structures in rock. Many researchers have developed theoretical criteria for rock failure with crack growth based on experimental observations. Numerically using cohesive zone model for brittle material with an assumption of some plasticity is found to be a good approach to predict the crack growth in rocks. The cohesive zone model is popularly used for fracture simulation in brittle materials, uses traction-separation law. The traction-separation law represents the material damage zone in front of the crack tip where the material elements are pulled apart. The extended finite element method (XFEM) enhanced the capability of the classical finite element method capturing the crack propagation problems. The important feature of XFEM is that, it can extend the crack without any remeshing which makes it suitable for fracture process analysis. The present paper combines XFEM approach with cohesive zone model (CZM) to analyze the crack growth for rock using ABAQUS. The results of the analysis are compared with the experiments carried out in the laboratory and with available literatures on crack growth in rocks. The present paper demonstrates different crack types (tensile/shear) that gets initiated from the pre-existing flaw with respect to the applied loading. The numerical model using ABAQUS shows a good agreement with the theoretical and experimental results while predicting the crack propagation.
机译:了解岩石中的故障模式和裂纹传播可以为岩石中各种结构的安全和经济设计提供有用的信息。基于实验观察,许多研究人员对岩石破坏具有裂纹增长的理论标准。用假设一些可塑性的脆性材料的数值使用脆性区域模型是一种预测岩石裂纹增长的良好方法。粘性区域模型普遍用于脆性材料的断裂模拟,使用牵引分离法。牵引 - 分离法表示裂缝尖端前面的材料损伤区,其中材料元件被拉开。扩展有限元方法(XFEM)增强了捕获裂纹传播问题的经典有限元方法的能力。 XFEM的重要特征是,它可以延长裂缝而无需任何倒闭,这使其适用于裂缝过程分析。本文将XFEM方法与粘性区模型(CZM)结合在一起,分析了ABAQUS的岩石裂纹增长。将分析结果与实验室中的实验进行比较,并在岩石中的裂纹生长的可用文献。本文演示了从预先存在的缺陷相对于施加的载荷引发的不同裂缝类型(拉伸/剪切)。使用ABAQU的数值模型与理论和实验结果的同时显示出良好的一致性,同时预测裂缝繁殖。

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