(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