Ice grown in DMSO or proline solutions at atmospheric pressure undergoes a kinetic roughening transition at -16.0 +/- 0.2 °C, yielding hexagonal facets without ice-active molecules and showing different growth versus melting kinetics.
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Kinetic roughening transition of ice crystals and its implications during recrystallization
Ice grown in DMSO or proline solutions at atmospheric pressure undergoes a kinetic roughening transition at -16.0 +/- 0.2 °C, yielding hexagonal facets without ice-active molecules and showing different growth versus melting kinetics.