Antisymmetric exchange in La-substituted BiFe0.5Sc0.5O3 system: symmetry adapted distortion modes approach

被引:20
作者
Khalyavin, Dmitry D. [1 ]
Salak, Andrei N. [2 ]
Manuel, Pascal [1 ]
Olekhnovich, Nikolai M. [3 ]
Pushkarev, Anatoly V. [3 ]
Radysh, Yury V. [3 ]
Fedorchenko, Alexey V. [4 ]
Fertman, Elena L. [4 ]
Desnenko, Vladimir A. [4 ]
Ferreira, Mario G. S. [2 ]
机构
[1] Rutherford Appleton Lab, ISIS Facil, Didcot OX11 0QX, Oxon, England
[2] Univ Aveiro, Dept Mat & Ceram Engn, CICECO, P-3810193 Aveiro, Portugal
[3] NAS Belarus, Sci Pract Mat Res Ctr, Minsk 220072, BELARUS
[4] NAS Ukraine, B Verkin Inst Low Temp Phys & Engn, UA-61103 Kharkov, Ukraine
来源
ZEITSCHRIFT FUR KRISTALLOGRAPHIE-CRYSTALLINE MATERIALS | 2015年 / 230卷 / 12期
关键词
antisymmetric exchange; multiferroics; perovskites; THERMODYNAMIC THEORY; WEAK FERROMAGNETISM;
D O I
10.1515/zkri-2015-1873
中图分类号
O7 [晶体学];
学科分类号
0702 ; 070205 ; 0703 ; 080501 ;
摘要
Neutron powder diffraction measurements on the 35 % La-substituted Bi1-xLaxFe0.5Sc0.5O3-composition revealed that the samples obtained under high-pressure (6 GPa) and high-temperature (1500 K) conditions crystalize into a distorted perovskite structure with the orthorhombic Pnma symmetry and the unit cell para-meters: a(0) = 5.6745(2) angstrom, b(0) = 7.9834(3) angstrom and c(0) = 5.6310(2) angstrom. A long-range magnetic ordering takes place below 220 K and implies a G-type magnetic structure with the moments 4.10(4)mu(B) per Fe aligned predominately along the orthorhombic c-axis. The space group representation theory using the orthorhombic symmetry yields four bi-linear coupling schemes for the magnetic order parameters imposed by antisymmetric exchange interactions. The couplings are analysed based on symmetry adapted distortion modes defined in respect of the undistorted cubic perovskite structure. The approach allows a quantitative estimation of the coupling strength. It is shown that the experimentally found spin configuration combines the magnetic order parameters coupled by the atomic displacement modes with the largest amplitudes. The results indicate that the antisymmetric exchange is the dominant anisotropic term which fully controls the direction of the Fe3+ spins in the distorted perovskite lattice.
引用
收藏
页码:767 / 774
页数:8
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