Structural stability and magnetic properties of Bi1-xLa(Pr)xFeO3 solid solutions

被引:32
作者
Karpinsky, D. V. [1 ,2 ]
Troyanchuk, I. O. [2 ]
Mantytskaya, O. S. [2 ]
Khomchenko, V. A. [3 ]
Kholkin, A. L. [1 ]
机构
[1] Univ Aveiro, CICECO Dept Ceram & Glass Engn, P-3810193 Aveiro, Portugal
[2] NAS Belarus, SSPA Sci Pract Mat Res Ctr, Minsk 220072, BELARUS
[3] Univ Coimbra, CEMDRX Dept Phys, Fac Sci & Technol, P-3004516 Coimbra, Portugal
关键词
Multiferroics; Morphotropic phase boundary; Phase transition; Phase diagram; RARE-EARTH; TRANSITION;
D O I
10.1016/j.ssc.2011.08.002
中图分类号
O469 [凝聚态物理学];
学科分类号
070205 ;
摘要
In this work, X-ray diffraction data taken on Bi1-xLaxFeO3 solid solutions are used to verify the following structural phase transitions: "polar rhombohedral-antipolar orthorhombic" at x approximate to 0.16 and "commensurate-incommensurate" within the orthorhombic phase at x approximate to 0.18. In contrast, in the Bi1-xPrxFeO3 series, the polar rhombohedral phase transforms into an antipolar orthorhombic one at x >= 0.13. The polar rhombohedral phase near the morphotropic phase boundary exhibits an isothermal transformation into an antipolar orthorhombic phase, though the transformation occurs much faster in the case of La-doped compounds. The incommensurate structural phase was not detected in Bi1-xPrxFeO3 solid solutions. The ternary structural phase diagram is constructed for (Bi, La, Pr)FeO3 systems. In addition, the polar rhombohedral phase exhibits a magnetic field-induced transition from the modulated antiferromagnetic state into a homogeneous weak ferromagnetic state whereas the antipolar phase is a weak ferromagnetic state in the absence of an external field. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1686 / 1689
页数:4
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