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Investigation of representing hysteresis in macroscopic models of two-phase flow in porous media using intermediate scale experimental data

机译:使用中等规模的实验数据研究多孔介质两相流宏观模型中的磁滞现象

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摘要

Incorporating hysteresis into models is important to accurately capture the two phase flow behavior when porous media systems undergo cycles of drainage and imbibition such as in the cases of injection and post-injection redistribution of CO2 during geological CO2 storage (GCS). In the traditional model of two-phase flow, existing constitutive models that parameterize the hysteresis associated with these processes are generally based on the empirical relationships. This manuscript presents development and testing of mathematical hysteretic capillary pressuresaturationrelative permeability models with the objective of more accurately representing the redistribution of the fluids after injection. The constitutive models are developed by relating macroscopic variables to basic physics of two-phase capillary displacements at pore-scale and void space distribution properties. The modeling approach with the developed constitutive models with and without hysteresis as input is tested against some intermediate-scale flow cell experiments to test the ability of the models to represent movement and capillary trapping of immiscible fluids under macroscopically homogeneous and heterogeneous conditions. The hysteretic two-phase flow model predicted the overall plume migration and distribution during and post injection reasonably well and represented the postinjection behavior of the plume more accurately than the nonhysteretic models. Based on the results in this study, neglecting hysteresis in the constitutive models of the traditional two-phase flow theory can seriously overpredict or underpredict the injected fluid distribution during post-injection under both homogeneous and heterogeneous conditions, depending on the selected value of the residual saturation in the nonhysteretic models.
机译:将滞后现象纳入模型对于在多孔介质系统经历排水和吸水循环时(例如在地质CO2储存(GCS)过程中注入和注入后再分布CO2的情况)准确捕获两相流行为非常重要。在传统的两相流模型中,参数化与这些过程相关的磁滞的现有本构模型通常基于经验关系。该手稿介绍了数学滞回毛细压力饱和相对渗透率模型的开发和测试,目的是更准确地表示注入后流体的重新分布。本构模型是通过将宏观变量与孔隙尺度和孔隙空间分布特性下的两相毛细管位移的基本物理学联系起来而开发的。在一些中等规模的流通池实验中,使用具有和不具有滞后作为输入的本构模型的建模方法,通过一些中等规模的流通池实验进行了测试,以测试模型在宏观上均质和非均质条件下代表不溶混流体的运动和毛细管捕集的能力。滞后两相流模型比非滞后模型更好地预测了整个羽流在注入期间和注入后的总体迁移和分布,并且更准确地表示了羽流的注入后行为。根据本研究的结果,在传统的两相流理论的本构模型中忽略滞后现象可能会严重地过高或过低地预测均质和非均质条件下后注入过程中的注入流体分布,具体取决于残差的选定值。非滞后模型中的饱和度。

著录项

  • 来源
    《Water resources research》 |2017年第1期|199-221|共23页
  • 作者单位

    Lawrence Berkeley Natl Lab, Energy Geosci Div, Berkeley, CA 94720 USA;

    Lawrence Berkeley Natl Lab, Energy Geosci Div, Berkeley, CA 94720 USA;

    Colorado Sch Mines, Ctr Expt Study Subsurface Environm Proc CESEP, Golden, CO 80401 USA|Univ Texas Austin, Bur Econ Geol, Jackson Sch Geosci, Austin, TX USA;

    Lawrence Berkeley Natl Lab, Energy Geosci Div, Berkeley, CA 94720 USA;

    Colorado Sch Mines, Ctr Expt Study Subsurface Environm Proc CESEP, Golden, CO 80401 USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    hysteresis; capillary trapping; two-phase flow;

    机译:磁滞;毛细管捕集;两相流;

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