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润湿性对多孔介质中动态流体连通性和流动传输动力学的影响

The Impact of Wettability on Dynamic Fluid Connectivity and Flow Transport Kinetics in Porous Media.

作者信息

Nhunduru Rumbidzai A E, Jahanbakhsh Amir, Shahrokhi Omid, Wlodarczyk Krystian L, Garcia Susana, Maroto-Valer M Mercedes

机构信息

School of Engineering and Physical Sciences Research Centre for Carbon Solutions (RCCS) Heriot-Watt University Edinburgh UK.

School of Engineering and Physical Sciences Applied Optics and Photonics (AOP) Group Heriot-Watt University Edinburgh UK.

出版信息

Water Resour Res. 2022 Jun;58(6):e2021WR030729. doi: 10.1029/2021WR030729. Epub 2022 Jun 3.

DOI:10.1029/2021WR030729
PMID:35859620
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9285789/
Abstract

Usually, models describing flow and transport for sub-surface engineering processes at the Darcy-scale do not take into consideration the effects of pore-scale flow regimes and fluid connectivity on average flow functions. In this article, we investigate the impact of wettability on pore-scale flow regimes. We show that fluid connectivity at the pore scale has a significant impact on average flow kinetics and therefore its contribution should not be ignored. Immiscible two-phase flow simulations were performed in a two-dimensional model of a Berea sandstone rock for wettability conditions ranging from moderately water-wet to strongly oil-wet. The simulation results show that wettability has a strong impact on invading fluid phase connectivity, which subsequently influences flow transport resistance. The effect of invading-phase connectivity and ganglion dynamics (GD) on two-phase displacement kinetics was also investigated. It was found that invading phase connectivity decreases away from the neutrally wet (intermediate wet) state. This study provides evidence that GD accelerate fluid flow transport kinetics during immiscible displacement processes. Lastly, the impact of wettability on fluid displacement efficiency and residual saturations was investigated. Maximum displacement efficiency occurred at the neutrally wet state.

摘要

通常，描述达西尺度下地下工程过程中流动与输运的模型并未考虑孔隙尺度流动状态和流体连通性对平均流动函数的影响。在本文中，我们研究了润湿性对孔隙尺度流动状态的影响。我们表明，孔隙尺度下的流体连通性对平均流动动力学有显著影响，因此其贡献不应被忽视。针对从适度水湿到强油湿的润湿性条件，在 Berea 砂岩的二维模型中进行了不混溶两相流模拟。模拟结果表明，润湿性对侵入流体相的连通性有强烈影响，进而影响流动输运阻力。还研究了侵入相连通性和节理动力学（GD）对两相驱替动力学的影响。发现侵入相连通性从中性湿润（中间湿润）状态开始降低。该研究提供了证据表明 GD 在不混溶驱替过程中加速流体流动输运动力学。最后，研究了润湿性对流体驱替效率和残余饱和度的影响。最大驱替效率出现在中性湿润状态。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6927/9285789/aa18fbbc567a/WRCR-58-0-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6927/9285789/bb155f2a5608/WRCR-58-0-g009.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6927/9285789/411c9b8db594/WRCR-58-0-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6927/9285789/74ee18d3f1af/WRCR-58-0-g007.jpg
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