The time domain-random walk method was developed further for simulating mass transfer in fracture flows together with matrix diffusion in surrounding porous media. Specifically, a time domain-random walk scheme was developed for numerically approximating solutions of the advection-diffusion equation when the diffusion coefficient exhibits significant spatial variation or even discontinuities. The proposed scheme relies on second-order accurate, central-difference approximations of the advective and diffusive fluxes. The scheme was verified by comparing simulated results against analytical solutions in flow configurations involving a rectangular channel connected on one side with a porous matrix. Simulations with several flow rates, diffusio...
The objective of this work is to discuss solute transport phenomena in fractured porous media, where...
AbstractAccurate descriptions of matrix diffusion across the fracture/matrix interface are critical ...
Solute transport in fractured porous media is typically 'non-Fickian'; that is, it is characterized ...
The time domain-random walk method was developed further for simulating mass transfer in fracture fl...
International audienceThe time domain random walk (TDRW) method has been developed for simulating so...
Multiscale features of transport processes in fractured porous media make numerical modeling a diffi...
The dual-continuum random-walk particle tracking approach is an attractive simulation method for sim...
International audienceRandom walk (RW) or Continuous Time Random Walk (CTRW) are recurring Monte Car...
The objective of this work is to discuss transport phenomena in fractured aquifers where the hydraul...
International audienceThe Time Domain Random Walk (TDRW) method has been recently developed by Delay...
International audienceSince the first attempts some 20 yr ago in the field of hydrology, random walk...
We study modeling of two-phase flow in highly heterogeneous fractured and porous media. The flow beh...
International audienceIn this study, new multi-dimensional time-domain random walk (TDRW) algorithms...
It is essential to study nuclide transport with underground water in fractured rock masses in order ...
Solute transport observed in subsurface formations shows complex behavior, particularly in the prese...
The objective of this work is to discuss solute transport phenomena in fractured porous media, where...
AbstractAccurate descriptions of matrix diffusion across the fracture/matrix interface are critical ...
Solute transport in fractured porous media is typically 'non-Fickian'; that is, it is characterized ...
The time domain-random walk method was developed further for simulating mass transfer in fracture fl...
International audienceThe time domain random walk (TDRW) method has been developed for simulating so...
Multiscale features of transport processes in fractured porous media make numerical modeling a diffi...
The dual-continuum random-walk particle tracking approach is an attractive simulation method for sim...
International audienceRandom walk (RW) or Continuous Time Random Walk (CTRW) are recurring Monte Car...
The objective of this work is to discuss transport phenomena in fractured aquifers where the hydraul...
International audienceThe Time Domain Random Walk (TDRW) method has been recently developed by Delay...
International audienceSince the first attempts some 20 yr ago in the field of hydrology, random walk...
We study modeling of two-phase flow in highly heterogeneous fractured and porous media. The flow beh...
International audienceIn this study, new multi-dimensional time-domain random walk (TDRW) algorithms...
It is essential to study nuclide transport with underground water in fractured rock masses in order ...
Solute transport observed in subsurface formations shows complex behavior, particularly in the prese...
The objective of this work is to discuss solute transport phenomena in fractured porous media, where...
AbstractAccurate descriptions of matrix diffusion across the fracture/matrix interface are critical ...
Solute transport in fractured porous media is typically 'non-Fickian'; that is, it is characterized ...