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Structural evolution of (Ca0.35Sr0.65)TiO3 perovskite at high pressures
Authors:Michael A. Carpenter  Susana Rios  Wilson Crichton
Affiliation:a University of Cambridge, Department of Earth Sciences, Downing Street, Cambridge CB2 3EQ, UK
b Departmento Física de la Materia Condensada, Facultad de Ciencia y Tecnología, Universidad del País Vasco, Apdo. 644, 48080 Bilbao, Spain
c ESRF, 6 Rue Jules Horowitz, BP 220, 38043 Grenoble CEDEX 9, France
d LEPMI-ENSEEG, 1130 Rue de la piscine, B.P. 75, 38042 St. Martin d’Hères, France
Abstract:Lattice parameters of a synthetic powder sample of Ca0.35Sr0.65TiO3 perovskite have been determined by the method of Le Bail refinement, using synchrotron X-ray diffraction patterns collected at pressures up to 15.5 GPa with a membrane-driven diamond anvil cell. At ambient conditions, diffraction data were consistent with the I4/mcm structure reported previously in the literature for the same composition. Diffraction data collected at high pressures were consistent with tetragonal (or, at least, pseudo-tetragonal) lattice geometry, and no evidence was found for the development of any of the orthorhombic structures identified in other studies of (Ca, Sr)TiO3 perovskites. Additional weak reflections, which could not be accounted for by the normal I4/mcm perovskite structure, were detected in diffraction patterns collected at pressures of 0.9-2.5 GPa, and above ∼13.5 GPa, however. Small anomalies in the evolution of unit cell volume and tetragonal strain were observed near 3 GPa, coinciding approximately with breaks in slope with increasing pressure of bulk and shear moduli for a sample with the same composition which had previously been reported. The anomalies could be due either to new tetragonal↔tetragonal/pseudo-tetragonal phase transitions or to subtle changes in compression mechanism of the tetragonal perovskite structure.
Keywords:Phase transitions   (Ca, Sr)TiO3   Perovskite   Landau theory   High pressure   Spontaneous strain
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