Articles | Volume 29, issue 20
https://doi.org/10.5194/hess-29-5625-2025
https://doi.org/10.5194/hess-29-5625-2025
Research article
 | 
22 Oct 2025
Research article |  | 22 Oct 2025

Linking chemical weathering, evolution of preferential flow paths and transport self-organization in porous media using non-equilibrium thermodynamics

Evgeny Shavelzon, Erwin Zehe, and Yaniv Edery

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Cited articles

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Al-Khulaifi, Y., Lin, Q., Blunt, M. J., and Bijeljic, B.: Pore-Scale Dissolution by CO2 Saturated Brine in a Multi-Mineral Carbonate at Reservoir Conditions: Impact of Physical and Chemical Heterogeneity, Water Resources Research, 55, 3171–3193, https://doi.org/10.1029/2018WR024137, 2019. a
Ben-Naim, A.: A Farewell to Entropy, World Scientific, 412 pp., https://doi.org/10.1142/6469, 2008. a
Ben-Naim, A.: Entropy, Shannon's Measure of Information and Boltzmann's H-Theorem, Entropy, 19, https://doi.org/10.3390/e19020048, 2017. a, b, c
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Short summary
We analyze how chemical reactions and fluid movement in porous materials interact, focusing on how water channels form in underground environments. Using a thermodynamic approach, we track energy dissipation due to fluid friction and chemical reaction, and correlate it with the intensity of the emerged water channels to understand this process. Over time, water channels become more defined, reducing energy dissipation due to mixing, reaction and fluid friction.
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