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Influence of capillary pressure gradient on connectivity of flow through a porous medium

机译:毛细管压力梯度对通过多孔介质的流动连通性的影响

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We study the nonlinear development of perturbations of the phase transition surface in the Hele-Shaw cell and a porous medium with a change of capillary pressure gradient along the interface. A bounded water-saturated region surrounded by humid air is explored. Capillary pressure at the interface causes deformation and movement of the water-saturated region. An approximate analytical solution using the method of characteristics is derived and compared with numerical simulation results. It is shown that the evolution of the deforming region can lead to its breakup into disconnected parts. Numerical experiments also show that the deformation of closely spaced separate regions can lead to their fusion. Such the reconfiguration of the interfaces can cause significant changes in the flow properties. Fragmentation during the motion and evaporation of groundwater leads to the formation of isolated inclusions of the substance carried by the water flow. (C) 2018 Elsevier Ltd. All rights reserved.
机译:我们研究了Hele-Shaw池和多孔介质中沿界面的相变表面扰动的非线性发展,其中多孔介质的毛细压力梯度发生了变化。探索了被潮湿空气包围的水饱和边界区域。界面处的毛细管压力导致水饱和区域变形和运动。推导了使用特征方法的近似解析解,并将其与数值模拟结果进行了比较。结果表明,变形区域的演变可以导致其分解为不连续的部分。数值实验还表明,相距很近的单独区域的变形会导致它们融合。接口的这种重新配置可能导致流量属性发生重大变化。地下水运动和蒸发过程中的碎裂导致水流携带的物质的孤立夹杂物的形成。 (C)2018 Elsevier Ltd.保留所有权利。

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