History independence of steady state in simultaneous two-phase flow through two-dimensional porous media

被引:33
|
作者
Erpelding, Marion [1 ]
Sinha, Santanu [2 ]
Tallakstad, Ken Tore [1 ]
Hansen, Alex [2 ]
Flekkoy, Eirik Grude [1 ]
Maloy, Knut Jorgen [1 ]
机构
[1] Univ Oslo, Dept Phys, N-0316 Oslo, Norway
[2] Norwegian Univ Sci & Technol, Dept Phys, N-7491 Trondheim, Norway
来源
PHYSICAL REVIEW E | 2013年 / 88卷 / 05期
关键词
DIFFUSION-LIMITED AGGREGATION; LATTICE-BOLTZMANN; RELATIVE PERMEABILITIES; MULTIPHASE FLOW; FRACTIONAL FLOW; SIMULATIONS; MODEL; DISPLACEMENTS; PERCOLATION; MECHANISMS;
D O I
10.1103/PhysRevE.88.053004
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
It is well known that the transient behavior during drainage or imbibition in multiphase flow in porous media strongly depends on the history and initial condition of the system. However, when the steady-state regime is reached and both drainage and imbibition take place at the pore level, the influence of the evolution history and initial preparation is an open question. Here, we present an extensive experimental and numerical work investigating the history dependence of simultaneous steady-state two-phase flow through porous media. Our experimental system consists of a Hele-Shaw cell filled with glass beads which we model numerically by a network of disordered pores transporting two immiscible fluids. From measurements of global pressure evolution, histograms of saturation, and cluster-size distributions, we find that when both phases are flowing through the porous medium, the steady state does not depend on the initial preparation of the system or on the way it has been reached.
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页数:12
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