This dataset includes the measured threshold gradients and permeabilities of low permeability porous at 3 temperatures, and the measured hydraulic gradients and flow velocities of different permeabilities at 3 temperatures. The experiment is designed to reveal the temperature effects on the non-Darcian flow in low permeability porous media
The flux of water through the hyporheic zone (HZ) is controlled by stream bedforms, sinuosity, surfa...
International audienceUnderstanding non-Darcian flow of shear-thinning fluids through rough-walled r...
Heat and mass transfer through porous media has been a topic of research interest because of its imp...
This dataset includes the measured threshold gradients and permeabilities of low permeability porous...
The permeability of a porous material represents the ability of the material to be crossed by a flui...
Low‐permeability porous medium usually has asymmetric distributions of pore sizes andpore‐throat tor...
This paper studies typical nonlinear models of fluid flow through multi-porous media in low-permeabi...
Heat transport in natural porous media, such as aquifers or streambeds, is generally modeled assumin...
One of the first objectives of this project was to design and build an experiment that could measure...
This work investigates the flow of fluid through a horizontal channel filled with a porous media wit...
The work presented concerns laminar flow through a porous media whose pore length scales vary in the...
The effect of various forms of nonuniform basic temperature gradients on the onset of convection in ...
A non-Darcy flow develops in porous media when the velocity of reservoir fluids becomes extremely hi...
The effect of various forms of nonuniform basic temperature gradients on the onset of convection in ...
This thesis examined the effect of sub-boiling temperatures on subsurface flow and mass transport, a...
The flux of water through the hyporheic zone (HZ) is controlled by stream bedforms, sinuosity, surfa...
International audienceUnderstanding non-Darcian flow of shear-thinning fluids through rough-walled r...
Heat and mass transfer through porous media has been a topic of research interest because of its imp...
This dataset includes the measured threshold gradients and permeabilities of low permeability porous...
The permeability of a porous material represents the ability of the material to be crossed by a flui...
Low‐permeability porous medium usually has asymmetric distributions of pore sizes andpore‐throat tor...
This paper studies typical nonlinear models of fluid flow through multi-porous media in low-permeabi...
Heat transport in natural porous media, such as aquifers or streambeds, is generally modeled assumin...
One of the first objectives of this project was to design and build an experiment that could measure...
This work investigates the flow of fluid through a horizontal channel filled with a porous media wit...
The work presented concerns laminar flow through a porous media whose pore length scales vary in the...
The effect of various forms of nonuniform basic temperature gradients on the onset of convection in ...
A non-Darcy flow develops in porous media when the velocity of reservoir fluids becomes extremely hi...
The effect of various forms of nonuniform basic temperature gradients on the onset of convection in ...
This thesis examined the effect of sub-boiling temperatures on subsurface flow and mass transport, a...
The flux of water through the hyporheic zone (HZ) is controlled by stream bedforms, sinuosity, surfa...
International audienceUnderstanding non-Darcian flow of shear-thinning fluids through rough-walled r...
Heat and mass transfer through porous media has been a topic of research interest because of its imp...
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