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A Micromechanical Model for Time Dependent Behavior Related to Subcritical Damage in Quasi Brittle Rocks

机译:准脆性岩石亚临界损伤的时变行为微力学模型

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In France,an underground research laboratory is constructed in a clay formation,called Callovo-Oxfordian argillites.In order to evaluate quantitatively the structure durability,it is necessary to achieve a good understanding of the long-term behavior of the material.Subcritical crack growth is one of main causes of time-dependent behavior in rock.In order to rigorous modeling of the time-dependent behavior of studied material,a micromechanicai model incorporated subcritical damage propagation is proposed for Callovo-Oxfordian argillites in this paper.In the proposed constitutive model,the argillite is considered as a two phase composite:the clay matrix and the mineral inclusion.Based on experimental observations [1],the clay matrix is described by a time-dependent damage model and the mineral inclusions are described by a linear elastic model.The passage from the micro-scale to the macro-scale is done through different homogenization schemes for studying their influences on the subcritical propagation of cracks.
机译:在法国,地下研究实验室是在粘土地层中建造的,称为卡洛沃-牛津泥质。为了定量评估结构的耐久性,有必要对材料的长期行为有一个很好的了解。岩石是时间相关行为的主要原因。为了对被研究材料的时间相关行为进行严格的建模,本文提出了一种结合了亚临界损伤传播的卡洛沃-牛津泥质微细观力学模型。模型中,将斜晶石视为粘土基体和矿物包裹体两相复合体。基于实验观察[1],粘土基体由时间相关的损伤模型描述,矿物包裹体由线性弹性描述。从微观尺度到宏观尺度的转变是通过不同的均化方案完成的,以研究它们对亚临界的影响裂纹的裂纹扩展。

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