Theory of ice premelting in porous media
Hendrik Hansen-Goos, J.S. Wettlaufer

TL;DR
This paper develops a comprehensive theoretical model for ice premelting in porous media, accounting for interfacial, grain boundary, impurity, and curvature effects to predict liquid water content below freezing.
Contribution
It introduces a unified equation for liquid fraction in porous ice, integrating multiple premelting mechanisms and impurity effects, advancing understanding of ice behavior in porous structures.
Findings
The model accurately predicts liquid water content at various temperatures.
Impurities and curvature significantly influence premelting extent.
The theory aligns with experimental observations in relevant settings.
Abstract
Premelting describes the confluence of phenomena that are responsible for the stable existence of the liquid phase of matter in the solid region of its bulk phase diagram. Here we develop a theoretical description of the premelting of water ice contained in a porous matrix, made of a material with a melting temperature substantially larger than ice itself, to predict the amount of liquid water in the matrix at temperatures below its bulk freezing point. Our theory combines the interfacial premelting of ice in contact with the matrix, grain boundary melting in the ice, and impurity and curvature induced premelting, the latter occurring in regions which force the ice-liquid interface into a high curvature configuration. These regions are typically found at points where the matrix surface is concave, along contact lines of a grain boundary with the matrix, and in liquid veins. Both…
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