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Constitutive Model and Damage Evolution of Mudstone under the Action of Dry-Wet Cycles

机译:干湿循环作用下泥岩的本构模型和损伤​​演化

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Mudstone is a natural type of geological material, which has different ways of mechanical response between natural state and dry-wet cycles. According to the complex damage theory of geological materials, rock masses can be considered as a composite material consisting of the structure phase and damage phase. The essence of the damage of rock masses is a damage evolution process, during which the deformation energy of the structure phase converts into dissipation energy of the damage phase, and the energy dissipation from phase transformation promotes the structure phase to change into the damage phase. In this study, a customized model test container and a novel test method are applied to study the decay rate of mudstone under different temperatures and over multiple dry-wet cycles. The decay rate and the damage variable are connected with each other and applied to the damage constitutive equation based on the energy principle to set up the damage evolution equation under the coupled action of dry-wet cycles and loads. Comparison of the proposed model with test results in a literature identifies the rationality of the established model and properly reflects the damage evolution of mudstone.
机译:泥岩是一种自然的地质材料,在自然状态和干湿循环之间具有不同的机械响应方式。根据地质材料的复杂破坏理论,岩体可以认为是由结构相和破坏相组成的复合材料。岩体破坏的实质是一个破坏演化过程,在此过程中,结构相的变形能转化为破坏相的耗散能,相变的能量耗散促使结构相转变为破坏相。在这项研究中,使用定制的模型测试容器和一种新颖的测试方法来研究泥浆在不同温度和多个干湿循环下的衰减率。衰减率与损伤变量相互联系,并基于能量原理应用于损伤本构方程,建立了干湿循环与载荷耦合作用下的损伤演化方程。将该模型与试验结果进行比较,可以确定所建立模型的合理性,并能正确反映泥岩的破坏演化。

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