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This is a Quantitative Study study.

October 16, 2025Open Access

Heat conduction with phase change in soils with macro-pores, snow, and cryoconite. Part I: unified model derivation and examples

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The study demonstrates a new model for thermal conduction across multiple scales, effectively addressing soils with macro-pores and snow.
Using established thermodynamic principles enhances the reliability of heat conduction predictions, particularly in permafrost environments.
The unified model links soil characteristics with bulk water models, effectively addressing complex scenarios in cryoconite regions.
This framework enables monolithic numerical simulations that couple soil and snow models, improving the understanding of thermal dynamics.

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This model extends heat conduction theory to soils, snow, and cryoconite, suggesting better heat transfer predictions.

Peszyńska et al. (2025) studied this question.

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