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Analysis of Damage and Permeability Evolution for Mudstone Material under Coupled Stress-Seepage

机译:耦合应力渗流下泥岩材料的损伤和渗透性演化分析

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摘要

Mudstone material in a deep roadway is under the coupled stress-seepage condition. To investigate the permeability change and damage development during rock excavation in roadways, a stress-seepage damage coupling model has been proposed. In this model, damage capacity expansion of mudstone material is considered as the initiation and propagation of micro-cracks and the fracture penetration. A damage variable is introduced into the proposed model based on the principle of minimum energy consumption. As a result, an elastoplastic damage constitutive equation is established. Then, the permeability evolution equation describing the micro-macro hydraulic behavior of mudstone is deduced via percolation theory, which can describe the characteristics of sudden permeability change after rock capacity expansion. Furthermore, a finite element model is established based on commercial finite element software-ABAQUS. The numerical model was firstly verified by comparison between experimental and simulation results. On the basis of it, numerical investigation of the temporal and spatial evolution law of pore pressure, damage and permeability coefficient during roadway excavation is undertaken. The numerical results indicate that with increase of construction time, pore pressure first increases and then decreases, while the damage zone and permeability coefficient increase gradually and finally nearly keep constant. The proposed coupling model and finite element method can describe damage and permeability evolution for mudstone material under coupled stress-seepage well.
机译:深道中的泥岩材料在耦合应力渗流条件下。为了探讨道路挖掘过程中的渗透性变化和损伤发展,提出了一种应力 - 渗流耦合模型。在该模型中,泥石材料的损伤能力膨胀被认为是微裂纹和裂缝渗透的起始和传播。基于最小能耗的原理,将损坏变量引入所提出的模型。结果,建立了弹性塑料损伤本构方程。然后,通过渗滤理论推导出描述泥岩微宏液压行为的渗透性演化方程,这可以描述岩石容量膨胀后突然渗透性变化的特性。此外,基于商业有限元软件-BAQUS建立有限元模型。通过实验和仿真结果的比较首先验证了数值模型。在其基础上,进行了沟道挖掘期间孔隙压力,损伤和渗透系数的时间和空间演化规律的数值研究。数值结果表明,随着施工时间的增加,孔隙压力首先增加,然后减少,而损伤区和渗透系数逐渐增加,最后几乎保持恒定。所提出的耦合模型和有限元方法可以描述耦合应力渗透下泥石材料的损伤和渗透性演化。

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