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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Bibliografiska uppgifter
I publikationen:Proc Natl Acad Sci U S A
Huvudupphovsmän: 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.
Materialtyp: Artigo
Språk:Inglês
Publicerad: National Academy of Sciences 2017
Ämnen:
Physical Sciences
Länkar: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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