Fluid-fluid interfacial area plays an important role for mass- and energy-transfer processes across the interface which is relevant in several hydrogeological and engineering applications, e.g. enhanced oil-gas recovery, CO2 storage in geological formations, unconventional geothermal systems, contaminant removal, etc. Kinetic interface sensitive tracers were designed to determine the size of the interface between two fluids by undergoing hydrolysis at the fluid-fluid interface. This study investigates by means of numerical modelling the influence of heterogeneity on the KIS tracer breakthrough curves in six idealized scenarios (S1-S6). It is an extension of the previous work conducted in “one-dimensional” column experiments by Tatomir et al...
We present experimental evidence of asymmetrical dispersive transport of a conservative tracer acros...
International audiencePorosity evolution at reactive interfaces is a key process that governs the ev...
Classical Darcy's equation for multiphase flow assumes that gravity and the gradient in fluid pressu...
Fluid-Fluid Interfacial Area (FIFA) is an important parameter relevant in numerous geological applic...
The quantification of the interfacial area between fluids in a multiphase system in porous media has...
Fluid-fluid interfacial area plays an important role for mass- and energy-transfer processes across ...
Two-phase flow in porous media is characterized by fluid-fluid interfaces that separate the fluid ph...
Recent computational studies of two-phase flow suggest that the role of fluid-fluid interfaces shoul...
Standard models of two-phase flow in porous media have been shown to exhibit several shortcomings th...
Many environmental issues deal with the movement of immiscible fluids in the subsurface, e.g., clean...
We perform pore-scale resolved direct numerical simulations of immiscible two-phase flow in porous m...
Wettability plays a vital role in many applications of flow in porous media and affects Darcy scale ...
An understanding of the pore-level interactions that affect multi-phase flow in porous media is impo...
Abstract: This paper systematically investigates the impact of porous mediadisorder and its coupling...
For the purpose of characterizing geologically stored $$\text{ CO}_{2}$$ including its phase partiti...
We present experimental evidence of asymmetrical dispersive transport of a conservative tracer acros...
International audiencePorosity evolution at reactive interfaces is a key process that governs the ev...
Classical Darcy's equation for multiphase flow assumes that gravity and the gradient in fluid pressu...
Fluid-Fluid Interfacial Area (FIFA) is an important parameter relevant in numerous geological applic...
The quantification of the interfacial area between fluids in a multiphase system in porous media has...
Fluid-fluid interfacial area plays an important role for mass- and energy-transfer processes across ...
Two-phase flow in porous media is characterized by fluid-fluid interfaces that separate the fluid ph...
Recent computational studies of two-phase flow suggest that the role of fluid-fluid interfaces shoul...
Standard models of two-phase flow in porous media have been shown to exhibit several shortcomings th...
Many environmental issues deal with the movement of immiscible fluids in the subsurface, e.g., clean...
We perform pore-scale resolved direct numerical simulations of immiscible two-phase flow in porous m...
Wettability plays a vital role in many applications of flow in porous media and affects Darcy scale ...
An understanding of the pore-level interactions that affect multi-phase flow in porous media is impo...
Abstract: This paper systematically investigates the impact of porous mediadisorder and its coupling...
For the purpose of characterizing geologically stored $$\text{ CO}_{2}$$ including its phase partiti...
We present experimental evidence of asymmetrical dispersive transport of a conservative tracer acros...
International audiencePorosity evolution at reactive interfaces is a key process that governs the ev...
Classical Darcy's equation for multiphase flow assumes that gravity and the gradient in fluid pressu...