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A simplified multiscale damage model for the transversely isotropic shale rocks under tensile loading

机译:横观各向同性页岩岩石在拉力作用下的简化多尺度损伤模型

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摘要

A simplified multiscale damage model is proposed for the transversely isotropic shale rocks under tensile loading. In this framework, the multiscale representations for the shale rocks are presented by introducing the microcrack-weakened equivalent solid with hierarchical microstructures, whose transversely isotropic properties are obtained by performing multilevel homogenization procedures. To simplify the calculation process for the damage-induced properties, the equivalent isotropic medium is attained by applying the Voigt–Reuss–Hill averaging process to the transversely isotropic solid. Subsequently, the microcrack-induced inelastic compliances are approximately derived in terms of microcrack opening displacements in the equivalent isotropic medium of the shale rock under tensile loading. The sizes and orientations of microcracks are taken as random variables. Both stationary and evolutionary damage models are considered. Microcrack kinetic equations are characterized through the use of a fracture mechanics-based stability criterion and microcrack geometry within a representative volume element. Numerical examples including experimental validations and comparisons with existing micromechanical models are presented to verify the proposed multiscale damage model. Finally, the influences of the silt inclusions and porosity on the material intrinsic and damage-induced properties are discussed.
机译:提出了横观各向同性页岩在拉力作用下的简化多尺度损伤模型。在此框架中,通过引入具有分层微观结构的微裂纹弱化的等效固体来表示页岩的多尺度表示,其横向各向同性特性是通过执行多级均质化程序获得的。为了简化损伤诱发特性的计算过程,通过对横观各向同性固体应用Voigt-Reuss-Hill平均过程获得等效各向同性介质。随后,根据拉力作用下页岩岩石当量各向同性介质中的微裂纹开口位移,近似推导了微裂纹引起的非弹性顺应性。微裂纹的大小和方向被视为随机变量。静态和进化损伤模型均被考虑。通过使用基于断裂力学的稳定性准则和代表性体积元素内的微裂纹几何形状来表征微裂纹动力学方程。数值示例包括实验验证和与现有微机械模型的比较,以验证所提出的多尺度损伤模型。最后,讨论了粉粒夹杂物和孔隙度对材料固有和损伤诱导性能的影响。

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