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A comparison between simulation and experiment for hysteretic phenomena during two-phase immiscible displacement

机译:两相不混溶位移过程中滞回现象的仿真与实验比较

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摘要

[1] The paper compares a theory for immiscible displacement based on distinguishing percolating and nonpercolating fluid parts with experimental observations from multistep outflow experiments. The theory was published in 2006 in Physica A, volume 371, pages 209-225; the experiments were published in 1991 in Water Resources Research, volume 27, pages 2113. The present paper focuses on hysteretic phenomena resulting from repeated cycling between drainage and imbibition processes in multistep pressure experiments. Taking into account, the hydraulic differences between percolating and nonpercolating fluid parts provides a physical basis to predict quantitatively the hysteretic phenomena observed in the experiment. While standard hysteretic extensions of the traditional theory are nonlocal in time the theory used in this paper is local in time. Instead of storing the pressure and saturation history, it requires only the current state of the system to reach the same quantitative agreement.
机译:[1]本文比较了基于区分渗流和非渗流流体部分的不混溶驱油理论,以及来自多步流出实验的实验观察结果。该理论发表于2006年的Physica A,第371卷,第209-225页;和该实验发表于1991年,水资源研究,第27卷,第2113页。本论文重点研究在多步压力实验中,排水和吸水过程之间反复循环而引起的滞后现象。考虑到,渗流和非渗流流体部分之间的水力差异为定量预测实验中观察到的滞后现象提供了物理基础。尽管传统理论的标准迟滞扩展在时间上是非局部的,但本文中使用的理论在时间上是局部的。无需存储压力和饱和历史记录,仅需要系统的当前状态即可达到相同的定量协议。

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  • 来源
    《Water resources research》 |2014年第1期|681-686|共6页
  • 作者

    F. Doster; R. Hilfer;

  • 作者单位

    Department of Civil and Environmental Engineering, Princeton University, Princeton, NJ 08544, USA,Department of Mathematics, Bergen University, Bergen, Norway;

    Institut fuer Computerphysik, Universitaet Stuttgart, Stuttgart, Germany,Institut fuer Physik, Universitaet Mainz, Mainz, Germany;

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