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Crystal structures and phases transitions of new double perovskite oxides Sr2-xCaxLnSbO6 (Ln= La, Sm and 0≤x≤1)

Abdessamad Faik ,  Edurne I. Zabalo ,  Irene U. Olabarria ,  Josu M. Igartua 

Facultad de Ciencia y Tecnología (UPV/EHU), P.Box 644, Bilbao 48080, Spain

Abstract

The perovskite structure type is one of the most regularly observed structure types in condensed matter sciences, as well as in advanced materials research and applications. This is due to their wide array of proprieties: superconducting, magnetoresistance,…. The double perovskite with general formula A2BB’O6 can be represented as a three-dimensional network of alternating BO6 and B’O6 octahedra, sharing the oxygens at the corners of the octahedra, with the A-cations occupying the interstitial spaces between the octahedra. The family of antimony double perovskite oxides with double perovskite has attracted a considerable attention because of the magnetic properties of some of its members, such as Sr2FeSbO6 [1,2].

The Sr2-xCaxLnSbO6 (Ln=La,Sm) (0≤x≤1) materials have been elaborated by the standard solid state reaction method. Rietveld analysis of laboratory x-ray powder diffraction data at room temperature, shows that these materials are double perovskite oxides and that should be represented by Sr2-xLnx[Ln1-xCax]SbO6 for 0≤x≤1, and by [Sr1-xCaxLn]CaSbO6 for 1≤x≤2, general formulas. In the lanthanum compounds, the A and B sites are totally occupied by La3+ and Ca2+ cations, respectively. In the samarium containing compounds, the Sm3+ and Ca2+ are partially disordered at the A and B. At room temperature, all these materials were found to have a monoclinic unit cell with a primitive space group P21/n. The high-temperature powder laboratory x-ray powder diffraction analysis has revealed that the most general temperature evolution of the crystal structures in these materials shows a double phase-transition sequence: from monoclinic (S.G. P21/n) to rhombohedral (S.G. R-3) and, then, to cubic symmetry (S.G. Fm-3m), with increasing of temperature. The transition temperatures increase as the size of the cation in the A-site decreases. Thus, the mechanism of these phase transition is related to the mistmatch between the size of the A cation and the cuboctahedral space between the BO6 and B’O6 octahedra.

[1] E.J. Cussen, J.F. Vente, P.D. Battle and T.C. Gibb (1997), J. Mater. Chem. 7 459-463. [2] N. Kashima, K. Inoue, T. Wada and Y. Yamaguchi (2002), Appl. Phys. A 74 S805-S807

 

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Presentation: Poster at 11th European Powder Diffraction Conference, Poster session, by Abdessamad Faik
See On-line Journal of 11th European Powder Diffraction Conference

Submitted: 2008-04-29 19:11
Revised:   2009-06-07 00:48