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dc.contributor.authorCartwright, Julyan H. E.-
dc.contributor.authorPiro, Oreste-
dc.contributor.authorSánchez, Pedro A.-
dc.contributor.authorSintes, Tomàs-
dc.date.accessioned2013-06-28T12:36:29Z-
dc.date.available2013-06-28T12:36:29Z-
dc.date.issued2012-12-27-
dc.identifierdoi: 10.1063/1.4772202-
dc.identifierissn: 0021-9606-
dc.identifiere-issn: 1089-7690-
dc.identifier.citationJournal of Chemical Physics 137: 244503 (2012)-
dc.identifier.urihttp://hdl.handle.net/10261/78803-
dc.description.abstractWe investigate ice polyamorphism in the context of the two-dimensional Mercedes-Benz model of water. We find a first-order phase transition between a crystalline phase and a high-density amorphous phase. Furthermore, we find a reversible transformation between two amorphous structures of high and low density; however, we find this to be a continuous and not an abrupt transition, as the low-density amorphous phase does not show structural stability. We discuss the origin of this behavior and its implications with regard to the minimal generic modeling of polyamorphism. © 2012 American Institute of Physics.-
dc.description.sponsorshipSimulations were performed at the IFISC’s Nuredduna highthroughput computing clusters, supported by the projects GRID-CSIC and FISICOS (FIS2007-60327, funded by the Spanish MINCNN and the ERDF). J.H.E.C. acknowledges MINCINN (Spain) Project No. FIS2010-22322-528C02-02. O.P. and P.A.S. acknowledge MINCINN (Spain) Project No. FIS2010-22322-528C02-01.-
dc.language.isoeng-
dc.publisherAmerican Institute of Physics-
dc.rightsopenAccess-
dc.titleIce polyamorphism in the minimal Mercedes-Benz model of water-
dc.typeartículo-
dc.identifier.doi10.1063/1.4772202-
dc.relation.publisherversionhttp://dx.doi.org/10.1063/1.4772202-
dc.date.updated2013-06-28T12:36:29Z-
dc.description.versionPeer Reviewed-
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