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Image-based modeling of spontaneous imbibition in porous media by a dynamic pore network model

机译:动态孔网模型多孔介质自发性吸收的基于图像的模型

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摘要

The dynamic pore-network modeling, as an efficient pore-scale tool, has been used to understand imbibition in porous media, which plays an important role in many subsurface applications. In this work, we aim to develop a dynamic pore-network model for imaged-based modeling of spontaneous imbibition in porous media. The mu CT scanning of a porous medium of sintered glass beads is selected as our study domain. We extract its pore network by using an open-source software of PoreSpy, and further project the extracted information of individual watersheds into multiform idealized pore elements. A number of case studies of primary spontaneous imbibition have been conducted by using both the pore-network model and a VOF model, under different wettability values and viscosity ratios. We compare those model predictions in terms of imbibition rates and temporal saturation profiles along the flow direction. We show that our pore-network model can well predict imbibition rates and temporal saturation profiles under different viscosity ratios and wetting conditions, in comparison to the VOF model. We explore the effect of viscosity ratio on the trapping of nonwetting phase. Moreover, we discuss the difference between spontaneous imbibition and quasi-static imbibition in terms of pore-filling mechanisms.
机译:作为一种有效的孔径工具,动态孔网络建模已被用于了解多孔介质中的吸收,这在许多地下应用中起着重要作用。在这项工作中,我们的目的是开发一种动态孔网络模型,用于多孔介质中的自发性吸收的基于成像的建模。选择烧结玻璃珠的多孔介质的MU CT扫描作为我们的研究结构域。我们通过使用Porespy的开源软件来提取其孔网络,并进一步将个别流域的提取信息投入到多个圆形的理想化孔元件中。通过使用孔网模型和VOF模型,在不同的润湿性值和粘度比下进行了许多对初级自发性吸收的案例研究。我们在沿着流动方向的吸入速率和时间饱和分布方面比较这些模型预测。我们表明,与VOF模型相比,我们的孔网模型可以在不同的粘度比和润湿条件下预测利用率和时间饱和型材。我们探讨了粘度比对非纯度阶段捕获的影响。此外,我们讨论了在孔填充机制方面的自发性吸收和准静态吸收之间的差异。

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  • 来源
    《Advances in Water Resources》 |2021年第6期|103932.1-103932.13|共13页
  • 作者单位

    Chongqing Univ State Key Lab Coal Mine Disaster Dynam & Control Chongqing Peoples R China|Chongqing Univ Sch Resources & Safety Engn Chongqing Peoples R China;

    Eindhoven Univ Technol Dept Mech Engn Eindhoven Netherlands;

    Swiss Fed Inst Technol Geothermal Energy & Geofluids Inst Geophys Zurich Switzerland|South Valley Univ Geol Dept Qena Egypt;

    Swiss Fed Inst Technol Dept Mech & Proc Engn Zurich Switzerland;

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