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Characterization of the hydromechanical behavior of argillaceous rocks with effective gas permeability under deviatoric stress

机译:偏应力下有效透气性泥质岩流体力学特性的表征

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The realization of nuclear waste storage in the deep geological formation will change the hydromechanical properties of the host rocks around the man-made openings due to the stress redistribution during the excavation stage and the variation of the hydraulic conditions during the open drift stage and the closure stage. This paper mainly presents an experimental study on the evolution of effective gas permeability of Callovo-Oxfordient argillaceous rocks during dehydration and rehydration processes and its variation under loading and unloading conditions. The experimental results show that effective gas permeability increases with the diminution of degree of saturation, and the logarithm of effective gas permeability is in quasi linear relation to saturation for the degree of saturation less than 90%. But effective gas permeability is not sensitive to the deviatoric stress, even if the deviator exceeds the damage threshold. The method of mercury intrusion has also been used in studying the microstructure of argillaceous rocks.
机译:由于在开挖阶段应力的重新分布以及在开放漂移阶段和闭合过程中水力条件的变化,在深部地质构造中实现核废料存储将改变人造开口周围的母岩的流体力学特性。阶段。本文主要研究Callovo-Oxfordient泥质岩在脱水和复水过程中有效气体渗透率的演化及其在装卸条件下的变化的实验研究。实验结果表明,当饱和度小于90%时,有效气体渗透率随饱和度的降低而增加,有效气体渗透率的对数与饱和度呈近似线性关系。但是,即使偏斜度超过损伤阈值,有效的气体渗透率对偏斜应力也不敏感。压汞法也已用于研究泥质岩石的微观结构。

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