Microscopic model and phase diagrams of the multiferroic perovskite manganites

被引:154
作者
Mochizuki, Masahito [1 ]
Furukawa, Nobuo [1 ,2 ]
机构
[1] Univ Tokyo, Dept Appl Phys, Japan Sci & Technol Agcy, Multiferro Project,ERATO,Bunkyo Ku, Tokyo 1138656, Japan
[2] Aoyama Gakuin Univ, Dept Math & Phys, Kanagawa 2298558, Japan
关键词
NEUTRON-DIFFRACTION; MAGNETIC-PROPERTIES; WEAK FERROMAGNETISM; DISTORTION; FEATURES; ELECTROMAGNONS; POLARIZATION; TRANSITION; EVOLUTION; PR;
D O I
10.1103/PhysRevB.80.134416
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Orthorhombically distorted perovskite manganites, RMnO3 with R being a trivalent rare-earth ion, exhibit a variety of magnetic and electric phases including multiferroic (i.e., concurrently magnetic and ferroelectric) phases and fascinating magnetoelectric phenomena. We theoretically study the phase diagram of RMnO3 by constructing a microscopic spin model, which includes not only the superexchange interaction but also the single-ion anisotropy (SIA) and the Dzyaloshinsky-Moriya interaction (DMI). Analysis of this model using the Monte Carlo method reproduces the experimental phase diagrams as functions of the R-ion radius, which contain two different multiferroic states, i.e., the ab-plane spin cycloid with ferroelectric polarization P parallel to a and the bc-plane spin cycloid with P parallel to c. The orthorhombic lattice distortion or the second-neighbor spin exchanges enhanced by this distortion exquisitely controls the keen competition between these two phases through tuning the SIA and DMI energies. This leads to a lattice-distortion-induced reorientation of P from a to c in agreement with the experiments. We also discuss spin structures in the A-type antiferromagnetic state, those in the cycloidal spin states, origin and nature of the sinusoidal collinear spin state, and many other issues.
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页数:22
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