
(PhysOrg.com) — A wide range of phenomena depend on ice – specifically, phase transitions during ice crystal surface melting. In this transition, which occurs near the melting point, the ice surface morphs into what is known as a quasi-liquid layer (QLL) – a thin layer of ice grains where the water molecules are not in rigid solid structure, yet not in the random order of liquid.
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The hidden nanoworld of ice crystals: Revealing the dynamic behavior of quasi-liquid layers
