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dc.contributorMaterials Science and Engineering Laboratory, Ceramics Division National Institute of Standards and Technology, Gaithersburg, MD USAen_US
dc.contributor.authorBurton, Benjamin P.
dc.contributor.otherbenjamin.burton@nist.goven_US
dc.date.accessioned2013-04-08T19:03:07Z
dc.date.accessioned2014-08-05T19:24:54Z
dc.date.available2013-04-08T19:03:07Z
dc.date.available2014-08-05T19:24:54Z
dc.date.issued2013-04-08
dc.identifier.citationChemical Geology Volume 225, Issues 3–4, 31 January 2006, Pages 222–229en_US
dc.identifier.urihttp://hdl.handle.net/11115/108
dc.description.abstractFirst principles phase diagram calculations were performed for the system NaCl–KCl. Plane-wave pseudopotential calculations of formation energies were used as a basis for fitting cluster expansion Hamiltonians, both with and without an approximation for the excess vibrational entropy (SVIB). Including SVIB dramatically improves the agreement between calculated and experimental phase diagrams: experimentally, the consolute point is {XC = 0.348, TC = 765 K}Exp; without SVIB, it is {XC = 0.46, TC ≈ 1630 K}Calc; with SVIB, it is {XC = 0.43, TC ≈ 930 K}Calc.en_US
dc.relation.urihttp://dx.doi.org/10.1016/j.chemgeo.2005.08.016en_US
dc.rightsAttribution-NonCommercial-ShareAlike 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/3.0/us/*
dc.subjectComputational File Repository Categories::Methods::First Principlesen_US
dc.titleNaCl–KCl: The role of excess vibrational entropyen_US
dc.typeDataseten_US


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