Interplay between capillary, gravity and viscous forces in unsaturated porous media gives rise to a range of complex flow phenomena affecting morphology, stability and dynamics of wetting and drainage fronts. Similar average phase contents may result in significantly different fluid distribution and patterns affecting macroscopic transport properties of the unsaturated medium. The formulation of general force balance within simplified pore spaces yields scaling relationships for motion of liquid elements in which gravitational force in excess of capillary pinning force scales linearly with viscous force. Displacement fluid front morphology is described using dimensionless force ratios expressed as Bond and Capillary numbers. The concise rep...
Liquid invasion into a porous medium is a phenomenon of great importance in both nature and technolo...
The invasion and subsequent flow of a nonwetting fluid (NWF) in a three-dimensional, unconsolidated ...
PACS. 47.20.Gv – Viscous instability. PACS. 47.54.+r – Pattern selection; pattern formation. PACS. 4...
The experimental and numerical results of the capillary-force-driven climb of wetting liquid in poro...
Multiphase flow through a porous medium involves complex interactions between capillarity, viscosity...
Abstract: Two-phase flow and capillarity phenomenon in porous solids are well known in physics and ...
International audienceWe report on results from primary drainage experiments on quasi-twodimensional...
This work concentrates on the flow properties when one fluid displaces another fluid in a network of...
We perform pore-scale resolved direct numerical simulations of immiscible two-phase flow in porous m...
Pore velocity-dependent dynamic contact angles provide a mechanism for explaining the formation of f...
Thesis: Ph. D., Massachusetts Institute of Technology, Department of Civil and Environmental Enginee...
The effect of drainage front morphology on gaseous diffusion through partially saturated porous medi...
The dynamics of the capillary climb of a wetting liquid into a porous medium that is opposed by grav...
[2] To explain the dynamic behavior of the matric potential at the wetting front of gravity driven f...
The analysis of the dynamics and stability of the wetting liquid capillary climb flow in the porous ...
Liquid invasion into a porous medium is a phenomenon of great importance in both nature and technolo...
The invasion and subsequent flow of a nonwetting fluid (NWF) in a three-dimensional, unconsolidated ...
PACS. 47.20.Gv – Viscous instability. PACS. 47.54.+r – Pattern selection; pattern formation. PACS. 4...
The experimental and numerical results of the capillary-force-driven climb of wetting liquid in poro...
Multiphase flow through a porous medium involves complex interactions between capillarity, viscosity...
Abstract: Two-phase flow and capillarity phenomenon in porous solids are well known in physics and ...
International audienceWe report on results from primary drainage experiments on quasi-twodimensional...
This work concentrates on the flow properties when one fluid displaces another fluid in a network of...
We perform pore-scale resolved direct numerical simulations of immiscible two-phase flow in porous m...
Pore velocity-dependent dynamic contact angles provide a mechanism for explaining the formation of f...
Thesis: Ph. D., Massachusetts Institute of Technology, Department of Civil and Environmental Enginee...
The effect of drainage front morphology on gaseous diffusion through partially saturated porous medi...
The dynamics of the capillary climb of a wetting liquid into a porous medium that is opposed by grav...
[2] To explain the dynamic behavior of the matric potential at the wetting front of gravity driven f...
The analysis of the dynamics and stability of the wetting liquid capillary climb flow in the porous ...
Liquid invasion into a porous medium is a phenomenon of great importance in both nature and technolo...
The invasion and subsequent flow of a nonwetting fluid (NWF) in a three-dimensional, unconsolidated ...
PACS. 47.20.Gv – Viscous instability. PACS. 47.54.+r – Pattern selection; pattern formation. PACS. 4...