Effect of combined Ca/Ti and Ca/Nb substitution on the crystal and magnetic structure of BiFeO3
[Display omitted] •Ca/Ti and Ca/Nb substitutions modify the antiferromagnetic structure of BiFeO3.•The cycloidal structure → canted structure transformation is studied.•Lattice defects contribute to the instability of the cycloidal antiferromagnetic order. Herein, we report on the crystal structure,...
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Published in | Journal of magnetism and magnetic materials Vol. 491; p. 165561 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Amsterdam
Elsevier B.V
01.12.2019
Elsevier BV |
Subjects | |
Online Access | Get full text |
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Summary: | [Display omitted]
•Ca/Ti and Ca/Nb substitutions modify the antiferromagnetic structure of BiFeO3.•The cycloidal structure → canted structure transformation is studied.•Lattice defects contribute to the instability of the cycloidal antiferromagnetic order.
Herein, we report on the crystal structure, magnetic and local ferroelectric properties of the Bi1−xCaxFe1−xTixO3 and Bi1−xCaxFe1−x/2Nbx/2O3 perovskites prepared by a solid state reaction method. It has been found that the Ca2+/Nb5+-containing series is characterized by a narrower concentration range (x ≤ 0.2) over which the acentric R3c structure specific to the pure BiFeO3 can be stabilized. The compositional variation in the critical concentration defining the polar/nonpolar (R3c/Pnma) phase boundary can be understood as related to the chemical modification-induced changes in the lattice spacing diminishing the stability of the a−a−a− tilting in favor of the a−b+a− one. Both the Ca2+/Ti4+ and Ca2+/Nb5+ substitutions ensure the suppression of a cycloidal antiferromagnetic order, thus leading to the formation of a weak ferromagnetic polar state. While this effect is proven to be associated with a composition-driven reduction in polar displacements, lattice defects are supposed to contribute to the instability of the cycloidal spin arrangement. |
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ISSN: | 0304-8853 1873-4766 |
DOI: | 10.1016/j.jmmm.2019.165561 |