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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Detalhes bibliográficos
Publicado no:Proc Natl Acad Sci U S A
Main Authors: 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.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2017
Assuntos:
Physical Sciences
Acesso em linha: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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