Two-phase flows in karstic geometry

被引:47
|
作者
Han, Daozhi [1 ]
Sun, Dong [1 ]
Wang, Xiaoming [1 ]
机构
[1] Florida State Univ, Dept Math, Tallahassee, FL 32306 USA
基金
美国国家科学基金会;
关键词
two-phase flow; diffusive interface model; phase-field model; karstic geometry; Onsager's extremum principle; energy law; time discretization; unique solvability; PHASE-FIELD MODEL; HELE-SHAW CELL; DIFFUSE INTERFACE MODEL; POROUS-MEDIA; IRREVERSIBLE-PROCESSES; RECIPROCAL RELATIONS; BOUNDARY-CONDITIONS; FINITE-DIFFERENCE; MULTIPHASE FLOW; STOKES;
D O I
10.1002/mma.3043
中图分类号
O29 [应用数学];
学科分类号
070104 ;
摘要
Multiphase flow phenomena are ubiquitous. Common examples include coupled atmosphere and ocean system (air and water), oil reservoir (water, oil, and gas), and cloud and fog (water vapor, water, and air). Multiphase flows also play an important role in many engineering and environmental science applications.In some applications such as flows in unconfined karst aquifers, karst oil reservoir, proton membrane exchange fuel cell, multiphase flows in conduits, and in porous media must be considered together. Geometric configurations that contain both conduit (or vug) and porous media are termed karstic geometry. Despite the importance of the subject, little work has been performed on multiphase flows in karstic geometry.In this paper, we present a family of phase-field (diffusive interface) models for two-phase flow in karstic geometry. These models together with the associated interface boundary conditions are derived utilizing Onsager's extremum principle. The models derived enjoy physically important energy laws. A uniquely solvable numerical scheme that preserves the associated energy law is presented as well. Copyright (c) 2013 John Wiley & Sons, Ltd.
引用
收藏
页码:3048 / 3063
页数:16
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