非饱和泥质岩石开挖损伤区水力渗透演化模型

B. Pardoen, S. Levasseur, F. Collin
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引用次数: 3

摘要

坑道的钻孔导致损伤在周围介质中传播,并形成开挖损伤区(EDZ),在该区域内材料性能发生改变。特别是在核废料地下储存的背景下,对该区域的裂缝结构和流动特性演化进行预测是一个重要的问题。由于实验结果表明剪切应变局部化出现在裂缝之前,我们使用耦合的局部二次梯度模型在剪切带模式下对EDZ进行应变局部化建模。考虑了裂隙内部水力渗透性的演化规律以及巷道通风对岩石失饱和的影响。数值结果提供了有关损伤区扩展、结构和行为的信息,与现场测量和观测结果有很好的对应关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Excavation damaged zone modelling including hydraulic permeability evolution in unsaturated argilaceous rock
The drilling of galleries induces damage propagation in the surrounding medium and creates the Excavation Damaged Zone (EDZ) in which the material properties are modified. The prediction of the fracture structure and flow properties evolution within this zone are major issues especially in the context of underground nuclear waste storage. Since experimental results indicate that shear strain localisation appears prior to fractures, we model the EDZ with strain localisation in shear band mode using the coupled local second gradient model. The evolution of the intrinsic hydraulic permeability inside the fractures is taken into consideration as well as the influence of gallery ventilation on the rock desaturation. The numerical results provide information about the damaged zone extension, structure and behaviour with good correspondence to in situ measurements and observations.
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