2013
DOI: 10.1016/j.ijmultiphaseflow.2012.12.006
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Evaluation of level set and phase field methods in modeling two phase flow with viscosity contrast through dual-permeability porous medium

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Cited by 161 publications
(50 citation statements)
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“…However, these "specialized" models cannot capture transitions between different regimes [18,31]. Grid-based methods with interface tracking such as volume of fluid (VOF) method and level set (LS) method have been proposed to study multiphase flow in porous media [32][33][34][35][36]. However, they suffer from numerical instability at the interface when interfacial tension becomes dominant for microdroplets [37].…”
Section: Introductionmentioning
confidence: 99%
“…However, these "specialized" models cannot capture transitions between different regimes [18,31]. Grid-based methods with interface tracking such as volume of fluid (VOF) method and level set (LS) method have been proposed to study multiphase flow in porous media [32][33][34][35][36]. However, they suffer from numerical instability at the interface when interfacial tension becomes dominant for microdroplets [37].…”
Section: Introductionmentioning
confidence: 99%
“…Popular methods for multiphase flow simulations include the volume of fluid [12] and level set [13] methods. More recently, the lattice Boltzmann technique, that belongs to the class of phase field methods, has shown its potential in the field of pore-scale multiphase fluid flow simulation [14].…”
Section: Introductionmentioning
confidence: 99%
“…The common goal in these approaches is to formulate thermodynamically consistent stress tensors and mesoscale balance laws, including the impact of surface tension on the momentum balance, as well as properly tracking interfacial dynamics [25]. Pore-scale modeling of immiscible two-phase flow using phase-field models has been done in [37][38][39]. We have successfully used the phase-field modeling framework to describe wetting and capillary phenomena in porous media, from unsaturated flow [40], thin films, and partial wetting [41,42] to pattern formation during immiscible displacement in Hele-Shaw flow [43].…”
Section: Introductionmentioning
confidence: 99%