A fundamental variable characterizing immiscible two-phase flow in porous media is the wetting saturation, which is the ratio between the pore volume filled with wetting fluid and the total pore volume. More generally, this variable comes from a specific choice of coordinates on some underlying space, the domain of variables that can be used to express the volumetric flow rate. The underlying mathematical structure allows for the introduction of other variables containing the same information, but which are more convenient from a theoretical point of view. We introduce along these lines polar coordinates on this underlying space, where the angle plays a role similar to the wetting saturation. We derive relations between these new variables ...
The phenomenology of steady-state two-phase flow in porous media is recorded in SCAL relative permea...
This thesis focuses primary on two-phase displacements under capillary-controlled flow conditions at...
Abstract. Flow of two immiscible, incompressible uids in a porous medium is typ-ically described by...
We present a theoretical framework for immiscible incompressible two-phase flow in homogeneous porou...
Models of instabilities in porous media usually assume that the capillary pressure (the difference o...
Flow of immiscible fluids in porous media at high capillary numbers may be characterized by an effec...
Models of instabilities in porous media usually assume that the capillary pressure (the difference o...
The impact of wettability on the co-moving velocity of two-fluid flow in porous media is analyzed he...
Thesis: S.M. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheric,...
We present a new numerical model for macroscale two-phase flow in porous media which is based on a p...
New equations for the two phase flow of water and steam are presented. The new equations coincide wi...
This article describes a semi-analytical model for two-phase immiscible flow in porous media. The mo...
Current theories of two-phase flow in porous media are based on the so-called extended Darcy’s law, ...
We construct a statistical mechanics for immiscible and incompressible two-phase flow in porous medi...
International audienceWe study experimentally the case of steady-state simultaneous two-phase flow i...
The phenomenology of steady-state two-phase flow in porous media is recorded in SCAL relative permea...
This thesis focuses primary on two-phase displacements under capillary-controlled flow conditions at...
Abstract. Flow of two immiscible, incompressible uids in a porous medium is typ-ically described by...
We present a theoretical framework for immiscible incompressible two-phase flow in homogeneous porou...
Models of instabilities in porous media usually assume that the capillary pressure (the difference o...
Flow of immiscible fluids in porous media at high capillary numbers may be characterized by an effec...
Models of instabilities in porous media usually assume that the capillary pressure (the difference o...
The impact of wettability on the co-moving velocity of two-fluid flow in porous media is analyzed he...
Thesis: S.M. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheric,...
We present a new numerical model for macroscale two-phase flow in porous media which is based on a p...
New equations for the two phase flow of water and steam are presented. The new equations coincide wi...
This article describes a semi-analytical model for two-phase immiscible flow in porous media. The mo...
Current theories of two-phase flow in porous media are based on the so-called extended Darcy’s law, ...
We construct a statistical mechanics for immiscible and incompressible two-phase flow in porous medi...
International audienceWe study experimentally the case of steady-state simultaneous two-phase flow i...
The phenomenology of steady-state two-phase flow in porous media is recorded in SCAL relative permea...
This thesis focuses primary on two-phase displacements under capillary-controlled flow conditions at...
Abstract. Flow of two immiscible, incompressible uids in a porous medium is typ-ically described by...