Abstract
Orthorhombically distorted perovskite manganites, with 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 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 -ion radius, which contain two different multiferroic states, i.e., the -plane spin cycloid with ferroelectric polarization and the -plane spin cycloid with . 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 from to in agreement with the experiments. We also discuss spin structures in the -type antiferromagnetic state, those in the cycloidal spin states, origin and nature of the sinusoidal collinear spin state, and many other issues.
12 More- Received 8 May 2009
DOI:https://doi.org/10.1103/PhysRevB.80.134416
©2009 American Physical Society