Different roles of surfaces’ interaction on lattice mismatched/matched surfaces in facilitating ice nucleation

Abstract

The freezing of water is one of the most common processes in nature and affects many aspects of human activity. Ice nucleation is a crucial part of the freezing process and usually occurs on material surfaces. There is still a lack of clear physical pictures about the central question how various features of material surfaces affect their capability in facilitating ice nucleation. Via molecular dynamics simulations, here we show that the detailed features of surfaces, such as atomic arrangements, lattice parameters, hydrophobicity, and function forms of surfaces’ interaction to water molecules, generally affect the ice nucleation through the average adsorption energy per unit-area surfaces to individual water molecules, while the lattice of surfaces mismatches that of ice. However, for the surfaces whose lattice matches ice, even the detailed function form of the surfaces’ interaction to water molecules can largely regulate the icing ability of these surfaces. This study provides new insights into understanding the diverse relationship between various microscopic features of different material surfaces and their nucleation efficacy.

Electric field as a crystallization switch of heterogeneous ice formation

“…However, some studies found that several materials with the same lattice as ice crystals, such as barium fluoride and cuprous bromide, are not effective heterogeneous ice nucleating materials [12,13]. Therefore, the lattice matching mechanism is insufficient to explain the ice nucleation on the substrate [14].…”