In this paper we study the structure of the ice/vapor interface in the neighborhood of the triple point for the TIP4P/2005 model. We probe the fluctuations of the ice/film and film/vapor surfaces that separate the liquid film from the coexisting bulk phases at basal, primary prismatic and secondary prismatic planes. The results are interpreted using a coupled sine Gordon plus Interface Hamiltonian model. At large length-scales, the two bounding surfaces are correlated and behave as a single complex ice/vapor interface. For small length, on the contrary, the ice/film and film/vapor surfaces behave very much like independent ice/water and water/vapor interfaces. The study suggests that the basal facet of the TIP4P/2005 model is smooth, the...
Ice crystal surfaces melt at temperatures below 0 °C, and then quasi-liquid layers (QLLs) are formed...
Ice surfaces are characterized by pre-melted quasi-liquid layers (QLLs), which mediate both crystal ...
Surface melting of ice crystals proceeds below the melting point (0 °C) and forms thin liquid water ...
In this paper we study the structure of the ice/vapor interface in the neighborhood of the triple po...
We perform computer simulations of the quasi-liquid layer of ice formed at the ice/vapor interface c...
Understanding the wetting properties of premelting films requires knowledge of the film’s equation o...
Using Lifshitz theory we assess the role of van der Waals forces at interfaces of ice and water. The...
ConspectusThe ice premelt, often called the quasi-liquid layer (QLL), is key for the lubrication of ...
Frozen water has a quasi-liquid layer at its surface that exists even well below the bulk melting te...
In this study, the solid-vapor equilibrium and the quasi liquid layer (QLL) of ice Ih exposing the b...
6 pags., 3 figs.Understanding the wetting properties of premelting films requires knowledge of the f...
We examine ice crystal growth from water vapor at temperatures near the melting point, when surface ...
Surfaces of ice are covered with thin liquid water layers, called quasi-liquid layers (QLLs), even b...
11 pags., 5 figs.Close to the triple point, the surface of ice is covered by a thin liquid layer (so...
We present measurements of the growth rates of the principal facet surfaces of ice from water vapor...
Ice crystal surfaces melt at temperatures below 0 °C, and then quasi-liquid layers (QLLs) are formed...
Ice surfaces are characterized by pre-melted quasi-liquid layers (QLLs), which mediate both crystal ...
Surface melting of ice crystals proceeds below the melting point (0 °C) and forms thin liquid water ...
In this paper we study the structure of the ice/vapor interface in the neighborhood of the triple po...
We perform computer simulations of the quasi-liquid layer of ice formed at the ice/vapor interface c...
Understanding the wetting properties of premelting films requires knowledge of the film’s equation o...
Using Lifshitz theory we assess the role of van der Waals forces at interfaces of ice and water. The...
ConspectusThe ice premelt, often called the quasi-liquid layer (QLL), is key for the lubrication of ...
Frozen water has a quasi-liquid layer at its surface that exists even well below the bulk melting te...
In this study, the solid-vapor equilibrium and the quasi liquid layer (QLL) of ice Ih exposing the b...
6 pags., 3 figs.Understanding the wetting properties of premelting films requires knowledge of the f...
We examine ice crystal growth from water vapor at temperatures near the melting point, when surface ...
Surfaces of ice are covered with thin liquid water layers, called quasi-liquid layers (QLLs), even b...
11 pags., 5 figs.Close to the triple point, the surface of ice is covered by a thin liquid layer (so...
We present measurements of the growth rates of the principal facet surfaces of ice from water vapor...
Ice crystal surfaces melt at temperatures below 0 °C, and then quasi-liquid layers (QLLs) are formed...
Ice surfaces are characterized by pre-melted quasi-liquid layers (QLLs), which mediate both crystal ...
Surface melting of ice crystals proceeds below the melting point (0 °C) and forms thin liquid water ...