Permeability changes of damaged rock salt adjacent to inclusions of different stiffness

Ishtiaque Anwar, M. Mills, E. Matteo, J. Stormont
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Abstract

Rock salt is being considered as a medium for energy storage and radioactive waste disposal. A Disturbed Rock Zone (DRZ) develops in the immediate vicinity of excavations in rock salt, with an increase in permeability, which alters the migration of gases and liquids around the excavation. When creep occurs adjacent to a stiff inclusion such as a concrete plug, it is expected that the stress state near the inclusion will become more hydrostatic and less deviatoric, promoting healing (permeability reduction) of the DRZ. In this study, we measured the permeability of DRZ rock salt with time adjacent to inclusions (plugs) of varying stiffness to determine how the healing of rock salt, as reflected in the permeability changes, is a function of stress and time. Samples were created with three different inclusion materials in a central hole along the axis of a salt core: (i) very soft silicone sealant, (ii) sorel cement, and (iii) carbon steel. The measured permeabilities are corrected for the gas slippage effect. We observed that the permeability change is a function of the inclusion material. The stiffer the inclusion, the more rapidly the permeability reduces with time.
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不同刚度包裹体相邻损伤岩盐的渗透率变化
岩盐正被考虑作为能量储存和放射性废物处理的介质。在岩盐中,随着岩盐渗透性的增加,在岩盐开挖附近形成了一个扰动岩带(DRZ),这改变了开挖周围气体和液体的运移。当蠕变发生在刚性包裹体(如混凝土塞)附近时,预计包裹体附近的应力状态将变得更静水,偏差更小,从而促进DRZ的愈合(渗透率降低)。在本研究中,我们测量了DRZ岩盐与不同刚度包裹体(塞)相邻时间的渗透率,以确定岩盐的愈合如何反映在渗透率变化中,这是应力和时间的函数。样品是用三种不同的包合材料在盐芯轴线上的中心孔中创建的:(i)非常柔软的硅酮密封胶,(ii)土壤水泥和(iii)碳钢。根据气体滑移效应对测量的渗透率进行了校正。我们观察到磁导率的变化是包合物的函数。夹杂物越硬,渗透率随时间降低的速度越快。
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