Porosity and Material Disorder Drive Distinct Channelization Transition

Fuente: arXiv
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Hauptverfasser: Matias, André F. V., Coelho, Rodrigo C. V., Carmona, Humberto A., Andrade Jr., José S., Araújo, Nuno A. M.
Format: Preprint
Veröffentlicht: 2026
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author Matias, André F. V.
Coelho, Rodrigo C. V.
Carmona, Humberto A.
Andrade Jr., José S.
Araújo, Nuno A. M.
author_facet Matias, André F. V.
Coelho, Rodrigo C. V.
Carmona, Humberto A.
Andrade Jr., José S.
Araújo, Nuno A. M.
contents Flow through porous media can reshape the medium through erosion and deposition, producing preferential flow channels across a wide range of natural and industrial systems. Yet the mechanisms by which spatial disorder triggers channelization remain unclear. Here we derive a continuum description for the coupled evolution of flow and porosity by coarse-graining pore-scale dynamics and validating the resulting model with pore-scale simulations. Using this framework, we show that different sources of disorder lead to qualitatively distinct behaviors. Disorder in erosion resistance produces a discontinuous transition to localized flow, with permanent channels appearing only above a finite disorder strength. In contrast, even extremely weak fluctuations in the initial porosity destabilize homogeneous flow and trigger persistent channelization. These results reveal an unexpected sensitivity of evolving porous media to structural heterogeneity, suggesting that channelization can arise generically even in nearly uniform materials.
format Preprint
id arxiv_https___arxiv_org_abs_2604_08025
institution arXiv
publishDate 2026
record_format arxiv
spellingShingle Porosity and Material Disorder Drive Distinct Channelization Transition
Matias, André F. V.
Coelho, Rodrigo C. V.
Carmona, Humberto A.
Andrade Jr., José S.
Araújo, Nuno A. M.
Fluid Dynamics
Soft Condensed Matter
Flow through porous media can reshape the medium through erosion and deposition, producing preferential flow channels across a wide range of natural and industrial systems. Yet the mechanisms by which spatial disorder triggers channelization remain unclear. Here we derive a continuum description for the coupled evolution of flow and porosity by coarse-graining pore-scale dynamics and validating the resulting model with pore-scale simulations. Using this framework, we show that different sources of disorder lead to qualitatively distinct behaviors. Disorder in erosion resistance produces a discontinuous transition to localized flow, with permanent channels appearing only above a finite disorder strength. In contrast, even extremely weak fluctuations in the initial porosity destabilize homogeneous flow and trigger persistent channelization. These results reveal an unexpected sensitivity of evolving porous media to structural heterogeneity, suggesting that channelization can arise generically even in nearly uniform materials.
title Porosity and Material Disorder Drive Distinct Channelization Transition
topic Fluid Dynamics
Soft Condensed Matter
url https://arxiv.org/abs/2604.08025