Continuum models that describe two-phase flow of immiscible fluids in porous media often treat momentum exchange between the two phases by simply generalizing the single-phase Darcy law and introducing saturation-dependent permeabilities. Here we study models of creeping flows that include an explicit coupling between both phases via the addition of cross terms in the generalized Darcy law. Using an extension of the Buckley-Leverett theory, we analyze the impact of these cross terms on saturation profiles and pressure drops for different couples of fluids and closure relations of the effective parameters. We show that these cross terms in the macroscale models may significantly impact the flow compared to results obtained with the generaliz...
The use of Darcy's law to describe steady-state multiphase flow in porous media has been justified b...
Thesis: S.M. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheric,...
Classical Darcy's equation for multiphase flow assumes that gravity and the gradient in fluid pressu...
The present work incorporates the effects of interface dynamics into the theoretical description of ...
The extended Darcy’s law is a commonly used equation for the description of immiscible two-phase flo...
International audienceHypothesisThe effects of mutual transfer of momentum between two immiscible fl...
Empirical or theoretical extensions of Darcy's law for immiscible two-phase flow have shown signific...
© The Author(s) 2011. This article is published with open access at Springerlink.com Abstract The ex...
Fluid-fluid momentum transfer can cause higher flow resistance when fluids flow in opposite directions a...
Abstract Problems involving flow in porous media are ubiquitous in many natural and engineered syste...
International audienceWe study experimentally the case of steady-state simultaneous two-phase flow i...
We present a new numerical model for macroscale two-phase flow in porous media which is based on a p...
Many industrial and natural processes involve flow in highly permeable media, such as exchangers, ca...
A fundamental variable characterizing immiscible two-phase flow in porous media is the wetting satur...
Traditionally, multiphase flow in porous media is described by the so-called extended Darcy’s Law, w...
The use of Darcy's law to describe steady-state multiphase flow in porous media has been justified b...
Thesis: S.M. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheric,...
Classical Darcy's equation for multiphase flow assumes that gravity and the gradient in fluid pressu...
The present work incorporates the effects of interface dynamics into the theoretical description of ...
The extended Darcy’s law is a commonly used equation for the description of immiscible two-phase flo...
International audienceHypothesisThe effects of mutual transfer of momentum between two immiscible fl...
Empirical or theoretical extensions of Darcy's law for immiscible two-phase flow have shown signific...
© The Author(s) 2011. This article is published with open access at Springerlink.com Abstract The ex...
Fluid-fluid momentum transfer can cause higher flow resistance when fluids flow in opposite directions a...
Abstract Problems involving flow in porous media are ubiquitous in many natural and engineered syste...
International audienceWe study experimentally the case of steady-state simultaneous two-phase flow i...
We present a new numerical model for macroscale two-phase flow in porous media which is based on a p...
Many industrial and natural processes involve flow in highly permeable media, such as exchangers, ca...
A fundamental variable characterizing immiscible two-phase flow in porous media is the wetting satur...
Traditionally, multiphase flow in porous media is described by the so-called extended Darcy’s Law, w...
The use of Darcy's law to describe steady-state multiphase flow in porous media has been justified b...
Thesis: S.M. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheric,...
Classical Darcy's equation for multiphase flow assumes that gravity and the gradient in fluid pressu...