Hydrated protons at the surface of water ice are of fundamental importance in a variety of physicochemical phenomena on earth and in the universe. Hydrated protons can be introduced by the autoionization of water molecules; thus, the autoionization and subsequent proton transfer processes determine the proton activity inherent to water molecular systems. A recent experimental study on the H/D isotopic exchange of water molecules reports markedly enhanced proton activity at the surface of crystalline ice.
Click here for original story, Unique structural fluctuations at ice surface promote autoionization of water molecules
Source: ScienceDaily