Forced Imbibition in Stratified Porous Media

Nancy B. Lu, A. Pahlavan, Christopher A. Browne, D. Amchin, H. Stone, S. Datta
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引用次数: 5

Abstract

Imbibition plays a central role in diverse energy, environmental, and industrial processes. In many cases, the medium has multiple parallel strata of different permeabilities; however, how this stratification impacts imbibition is poorly understood. We address this gap in knowledge by directly visualizing forced imbibition in three-dimensional (3D) porous media with two parallel strata. We find that imbibition is spatially heterogeneous: for small capillary number Ca, the wetting fluid preferentially invades the fine stratum, while for Ca above a threshold value, the fluid instead preferentially invades the coarse stratum. This threshold value depends on the medium geometry, the fluid properties, and the presence of residual wetting films in the pore space. These findings are well described by a linear stability analysis that incorporates crossflow between the strata. Thus, our work provides quantitative guidelines for predicting and controlling flow in stratified porous media.
层状多孔介质中的强制渗吸
渗吸在各种能源、环境和工业过程中起着核心作用。在许多情况下,介质具有多个渗透率不同的平行地层;然而,人们对这种分层如何影响渗吸知之甚少。我们通过直接可视化具有两个平行地层的三维(3D)多孔介质中的强迫渗吸来解决这一知识空白。研究发现,微吸在空间上是不均匀的,当毛管数Ca较小时,润湿流体优先侵入细粒地层,而当毛管数Ca大于阈值时,润湿流体优先侵入粗粒地层。该阈值取决于介质的几何形状、流体性质以及孔隙空间中是否存在残留的润湿膜。这些发现很好地描述了线性稳定性分析,包括地层之间的横流。因此,我们的工作为预测和控制分层多孔介质中的流动提供了定量指导。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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