Homogeneous nucleation of phase transformations in supercooled water
Robert Felix Tournier

TL;DR
This paper develops a thermodynamic model for phase transformations in supercooled water, explaining the fragile-to-strong transition and predicting properties consistent with experimental data across pressures.
Contribution
It introduces a new enthalpy-based nucleation model that accurately predicts water's phase behavior and transitions, including the fragile-to-strong transition, from known thermodynamic parameters.
Findings
Predicts the fragile-to-strong transition at TLL = 228.5 K.
Describes the formation of a glacial phase at TLL = 0.8367*Tm.
Explains the first-order transition without latent heat at TK2 = 122.4 K.
Abstract
The classical nucleation equation, applied to two liquids, is completed by an additional enthalpy for solid supercluster formation governing the liquid and glass transformations. This model, successfully applied to d-mannitol, triphenyl phosphite and n-butanol, defines a formation rule of strong glacial phase, explaining the origin of the first-order transition of water from fragile-to-strong liquid at TLL = 228.5 K, only knowing Tg = 137.1 K, the melting heat and the melting temperature Tm. All thermodynamic properties and transitions, even under pressure P, are now predicted in agreement with experiments of Kanno and Angell (1979), Mishima (1994), Mishima and Stanley (1998), Loerting et al (2006), Amann-Winkel et al (2013), Shephard and Salzmann (2016, 2017), Tulk et al (2019). This glacial phase is formed at TLL = 0.8367*Tm for P < 0.017 GPa. (TLL) decreases with P < 0.017 GPa and…
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