Experimental and theoretical evidence for bilayer-by-bilayer surface melting of crystalline ice

On the surface of water ice, a quasi-liquid layer (QLL) has been extensively reported at temperatures below its bulk melting point at 273 K. Approaching the bulk melting temperature from below, the thickness of the QLL is known to increase. To elucidate the precise temperature variation of the QLL,...

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Veröffentlicht in:Proc Natl Acad Sci U S A
Hauptverfasser: Sánchez, M. Alejandra, Kling, Tanja, Ishiyama, Tatsuya, van Zadel, Marc-Jan, Bisson, Patrick J., Mezger, Markus, Jochum, Mara N., Cyran, Jenée D., Smit, Wilbert J., Bakker, Huib J., Shultz, Mary Jane, Morita, Akihiro, Donadio, Davide, Nagata, Yuki, Bonn, Mischa, Backus, Ellen H. G.
Format: Artigo
Sprache:Inglês
Veröffentlicht: National Academy of Sciences 2017
Schlagworte:
Physical Sciences
Online Zugang:https://ncbi.nlm.nih.gov/pmc/articles/PMC5240679/
https://ncbi.nlm.nih.gov/pubmed/27956637
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1612893114
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