Anomalous Transport in Dissolving Porous Media: Transitions Between Fickian and Non‐Fickian Regimes
Abstract Mineral dissolution is a fundamental geologic process that alters pore structures, significantly impacting fluid flow and solute transport in porous media. Depending on the interplay between advection, diffusion, and reaction rates, mineral dissolution produces distinct dissolution patterns...
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| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Wiley
2025-08-01
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| Series: | Geophysical Research Letters |
| Online Access: | https://doi.org/10.1029/2025GL115940 |
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