Melting of orientational degrees of freedom

We use calorimetry and dilatometry under hydrostatic pressure, X-ray powder diffraction and available literature data in a series of composition-related orientationally disordered (plastic) crystals to characterize both the plastic and melting transitions and investigate relationships between associ...

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Detalles Bibliográficos
Autores: Aznar Luque, Araceli|||0000-0002-1499-0004, Lloveras Muntané, Pol Marcel|||0000-0003-4133-2223, Barrio Casado, María del|||0000-0003-3467-7581, Tamarit Mur, José Luis|||0000-0002-7965-0000
Tipo de recurso: artículo
Fecha de publicación:2017
País:España
Institución:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/105255
Acceso en línea:https://hdl.handle.net/2117/105255
https://dx.doi.org/10.1140/epjst/e2016-60315-4
Access Level:acceso abierto
Palabra clave:Calorimetry
X-rays -- Diffraction
Plastics
Calorimetria
Raigs X -- Difracció
Plàstics
Àrees temàtiques de la UPC::Física
Descripción
Sumario:We use calorimetry and dilatometry under hydrostatic pressure, X-ray powder diffraction and available literature data in a series of composition-related orientationally disordered (plastic) crystals to characterize both the plastic and melting transitions and investigate relationships between associated thermodynamic properties. First, general common trends are identified: (i) The temperature range of stability of the plastic phase Tm-Tt (where Tt and Tm are the plastic and melting transition temperatures, respectively) increases with increasing pressure and (ii) both the rate of this increase, d(Tm-Tt)/dp, and the entropy change across the plastic transition analyzed as function of the ratio Tt/Tm are quite independent of the particular compound. However, the dependence of the entropy change at the melting transition on Tt/Tm at high pressures deviates from the behavior observed at normal pressure for these and other plastic crystals. Second, we find that the usual errors associated with the estimations of second-order contributions in the Clausius-Clapeyron equation are high and thus these terms can be disregarded in practice. Instead, we successfully test the validity of the Clausius-Clapeyron equation at high pressure from direct measurements. References