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Magnetic Properties of the Bi6Fe2Ti3O18 Aurivillius Phase Prepared by Hydrothermal Method

Journal Advances in Science and Technology (Volume 67)
Volume 12th INTERNATIONAL CERAMICS CONGRESS PART F
Edited by Pietro VINCENZINI, Vojislav V. MITIC, Alois LOIDL and Dino FIORANI
Pages 170-175
DOI 10.4028/www.scientific.net/AST.67.170
Citation Mirosław M. Bućko et al., 2010, Advances in Science and Technology, 67, 170
Online since October, 2010
Authors Mirosław M. Bućko, Joanna Polnar, Janusz Przewoźnik, Jan Żukrowski, Czesław Kapusta
Keywords Aurivillius Phase, Bi6Fe2Ti3O18, Hydrothermal Synthesis, Magnetic Properties, Multiferroic
Abstract

The multiferroic Aurivillius phases in the Bi-Fe-Ti-O system are built from alternate (Bi2O2)2+ and (Bin-1XnO3n+1)2 layers, where X = Fe3+, Ti4+ and “n” refers to the number of perovskite-like layers between Bi2O2 layers. Detailed magnetic studies should be done to understand electromagnetic interactions and multiferroic coupling effects. In the present paper, a powder composed of the Aurivillius phase with n = 5, Bi6Fe2Ti3O18, was successfully prepared by the hydrothermal method. The powder was sintered, obtaining dense polycrystalline materials. It was stated that both powder and sintered bodies were paramagnets with a possible antiferromagnetic ordering or a spin-glass state at the liquid helium temperatures.

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