Abstract
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, diffusion coefficients, and matrix porosities indicate good agreement between the numerical approximations and analytical solutions.
| Original language | English |
|---|---|
| Pages (from-to) | 953–967 |
| Number of pages | 15 |
| Journal | Computational Geosciences |
| Volume | 23 |
| Issue number | 5 |
| DOIs | |
| Publication status | Published - 2019 |
| Publication type | A1 Journal article-refereed |
Funding
Financial support from the Finnish Research Programme on Nuclear Waste Management (KYT2018) is gratefully acknowledged. Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Keywords
- Advection
- Breakthrough curve
- Matrix diffusion
- Porous media
- Simulation
- Solute transport
Publication forum classification
- Publication forum level 1
ASJC Scopus subject areas
- Computer Science Applications
- Computers in Earth Sciences
- Computational Theory and Mathematics
- Computational Mathematics
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