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

• Malgorzata Peszynska ^[1] ; Praveeni Mathangadeera ^[1] ; Madison Phelps ^[1] ; Forrest Felsch ^[1] ; Noah Unger-Schulz ^[1]
  1. [1] Oregon State University

     Oregon State University

     Estados Unidos

     
• Localización: SeMA Journal: Boletín de la Sociedad Española de Matemática Aplicada, ISSN-e 2254-3902, ISSN 2254-3902, Vol. 82, Nº. Extra 4, 2025 (Ejemplar dedicado a: 28 CEDYA/ 18 CMA SeMA Congress), págs. 595-632
• Idioma: inglés
• DOI: 10.1007/s40324-025-00400-z
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• Resumen

  • In this paper we extend models of thermal conduction with phase transition from micro- to macro-scale. Such models were previously developed for soils in permafrost regions from pore to Darcy scale, and the Darcy scale models compare well to empirical relationships. The new general model blends soil model with bulk water model and thus works well for the soils with macro-pores; it also applies to new context including modeling thermal conduction in the snow and in cryoconite, and it is consistent with rigorous thermodynamics derivations as well as with practical models from the literature. From mathematical point of view, the general model relies on carefully defined relationships between temperature, phase fraction and internal energy, which we show are invertible in a properly defined framework of multivalued graphs. We also discuss and test practical models for average heat conductivity. Our framework allows to create monolithic numerical models useful for modeling of coupled soil and snow models as well as cryoconite. We motivate and illustrate the results with practical examples and computations.