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Stress-induced permeability changes in Indiana limestone

机译:应力引起的印第安纳石灰石渗透率变化

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This paper examines the influence of triaxial stress states with confining stresses between 5 and 30 MPa, including post-failure, on the alteration of intrinsic permeability of Indiana Limestone. The permeating fluid used in the experiments was distilled/de-aired water. Experimental results are used to develop an empirical state space model of permeability evolution due to the action of maximum and minimum principal stresses imposed on the sample. The developed empirical model is implemented in a computational code to examine the influence of stress-induced permeability alterations on the flow into an unlined cylindrical cavity located in a rock mass subjected to geostatic stresses. (C)2016 Elsevier B.V. All rights reserved.
机译:本文研究了在5到30 MPa范围内的三轴应力状态(包括破坏后)对印第安纳州石灰石固有渗透率变化的影响。实验中使用的渗透液是蒸馏水/去气水。由于施加在样品上的最大和最小主应力的作用,实验结果被用于建立渗透率演变的经验状态空间模型。所开发的经验模型以计算代码实现,以检查应力引起的渗透率变化对流入位于承受地应力的岩体中的无衬里圆柱腔内流动的影响。 (C)2016 Elsevier B.V.保留所有权利。

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