Abstract

The freezing of water is greatly influenced by the ice–water interfacial free energy. Yet, no consistent experimental measures of this thermodynamic parameter can be found. In this work we provide estimates for the ice Ih–water interfacial free energy at the normal melting temperature for different crystal planes (basal, primary prismatic, and secondary prismatic) using some widely used water models: TIP4P, TIP4P/2005, TIP4P/Ice, and mW. To compute the interfacial free energy, we use the mold integration method. It consists in calculating the work needed to induce the formation of a crystal slab in the fluid at coexistence conditions with the aid of a mold of potential energy wells whose structure is that of the crystal plane under study. The basal plane has the lowest interfacial free energy in all models of the TIP4P family. For the mW model we could not resolve differences in interfacial free energy between different orientations. The interfacial free energies averaged over all crystal orientations we ...

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