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Phase field modeling of brittle compressive-shear fractures in rock-like materials: A new driving force and a hybrid formulation

机译:岩石材料中脆性压剪断裂的相场模拟:新的驱动力和混合公式

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Compressive-shear fracture is commonly observed in rock-like materials. However, this fracture type cannot be captured by current phase field models (PFMs), which have been proven an effective tool for modeling fracture initiation, propagation, coalescence, and branching in solids. The existing PFMs also cannot describe the influence of cohesion and internal friction angle on load-displacement curve during compression tests. Therefore, to develop a new phase field model that can simulate well compressive-shear fractures in rock-like materials, we construct a new driving force in the evolution equation of phase field. Strain spectral decomposition is applied and only the compressive part of the strain is used in the new driving force with consideration of the influence of cohesion and internal friction angle. For ease of implementation, a hybrid formulation is established for the phase field modeling. Then, we test the brittle compressive-shear fractures in uniaxial compression tests on intact rock-like specimens as well as those with a single or two parallel inclined flaws. All numerical results are in good agreement with the experimental observation, validating the feasibility and practicability of the proposed PFM for simulating brittle compressive-shear fractures. (C) 2019 Elsevier B.V. All rights reserved.
机译:在岩石状材料中通常观察到压缩剪切断裂。但是,当前的相场模型(PFM)无法捕获这种裂缝类型,目前的相场模型已被证明是对固体中裂缝的发生,扩展,合并和分支进行建模的有效工具。现有的PFM还不能描述压缩试验期间内聚力和内摩擦角对载荷-位移曲线的影响。因此,为了建立一个新的能够模拟岩石状材料的压剪裂缝的相场模型,我们在相场的演化方程中构造了一个新的驱动力。考虑到内聚力和内摩擦角的影响,应用应变谱分解,并且在新的驱动力中仅使用应变的压缩部分。为了易于实施,建立了用于相场建模的混合公式。然后,我们在完整的岩石样试样以及具有单个或两个平行倾斜裂纹的试样的单轴压缩试验中测试脆性压缩剪切断裂。所有数值结果与实验结果吻合良好,验证了所提出的PFM模拟脆性压剪断裂的可行性和实用性。 (C)2019 Elsevier B.V.保留所有权利。

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