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Adaptive phase field simulation of quasi-static crack propagation in rocks

机译:岩石准静态裂纹扩展的自适应相场模拟

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In this study, we present an adaptive phase field method (APFM) for modeling quasi-static crack propagation in rocks. Crack initiation due to positive strains is considered, and a numerical simulation is implemented using a commercial software, COMSOL Multiphysics. Two benchmark tests are first examined, namely, a single-edge-notched square plate subjected to respective tension and shear loadings. The crack propagation in Brazil splitting tests, 2D notched semi-circular bend (NSCB) tests, and 3D NSCB tests are subsequently simulated and analyzed. All the numerical examples indicate that the propagation of the cracks is autonomous and external fracture criteria are not required for phase field modeling. Furthermore, the adaptive remeshing scheme reduces unnecessary global mesh refinement and exhibits good adaptability for fracture modeling. The simulations are in good agreement with the experimental observations, and thereby indicate the feasibility and practicability of the APFM in rocks (even in 3D cases).
机译:在这项研究中,我们提出了一种用于模拟岩石中准静态裂纹扩展的自适应相场方法(APFM)。考虑到由正应变引起的裂纹萌生,并使用商业软件COMSOL Multiphysics进行了数值模拟。首先检查两个基准测试,即承受相应拉力和剪切载荷的单边缺口方形板。随后模拟和分析了巴西劈裂测试,2D缺口半圆弯曲(NSCB)测试和3D NSCB测试中的裂纹扩展。所有数值实例表明,裂纹的扩展是自主的,相场建模不需要外部断裂准则。此外,自适应重划方案减少了不必要的全局网格细化,并显示出对裂缝建模的良好适应性。模拟与实验观察结果非常吻合,从而表明了APFM在岩石中的可行性和实用性(即使在3D情况下)。

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