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

被引:5
作者
Doster, F. [1 ,2 ]
Hilfer, R. [3 ,4 ]
机构
[1] Princeton Univ, Dept Civil & Environm Engn, Princeton, NJ 08544 USA
[2] Univ Bergen, Dept Math, N-5007 Bergen, Norway
[3] Univ Stuttgart, Inst Comp Phys, D-70174 Stuttgart, Germany
[4] Johannes Gutenberg Univ Mainz, Inst Phys, Mainz, Germany
关键词
two-phase flow; porous media; hysteresis; GOVERNING MULTIPHASE FLOW; POROUS-MEDIA; MACROSCOPIC CAPILLARITY; SATURATION; PRESSURE; MODEL;
D O I
10.1002/2013WR014619
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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.
引用
收藏
页码:681 / 686
页数:6
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