层状多孔介质中两相流动的界面动力学

Aniket S. Ambekar, V. Buwa, J. Phirani
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引用次数: 1

摘要

非润湿流体与润湿流体的非混相驱替对于许多领域都很重要,例如生物医学设备、纸微流体、油藏和含水层。在多层多孔介质中,各层之间的位移速度和相对位置是决定流体流动路径的重要因素。早期对两层多孔介质的研究表明,随速度的不同,每一层都存在不同的流动形式。然而,这些层在不同流型中相对位置的影响仍然是未知的。在本研究中,我们通过实验表明,在低速下,湿流体前缘在渗透率最低的层中超前,而在高速下,湿流体前缘在渗透率最高的层中超前。在所有流速下,由于毛细吸力的作用,最不渗透层从高渗透层中吸取流体。我们还展示了层的相对位置对相间动力学的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Interface Dynamics During Two Phase Flow in Stratified Porous Medium
Immiscible displacement of a non-wetting fluid by a wetting fluid is important for many fields for example, biomedical devices, paper micro-fluidics, oil reservoirs and water aquifers. In a multi-layered porous medium the displacement velocity and relative position of the layers with respect to each other is significant in determining the flow paths of the fluids. Earlier studies on two-layered porous medium indicate presence of different flow regimes in every layer depending upon the velocity. However, the effect of relative positioning of these layers in different flow regimes is still unknown. In the present work we experimentally show that at low velocity, a capillary regime is developed i.e. the wetting fluid front leads in the least permeable layer, while at high velocity the wetting fluid front leads in the highest permeability layer. At all flow rates, the least permeable layer is found to draw fluid from the high permeability layer due to capillary suction. We also show the effect of relative placement of the layers on the interphase dynamics.
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