Magnetoelectric phase diagrams of orthorhombic RMnO3 (R=Gd, Tb, and Dy)

被引:653
作者
Kimura, T [1 ]
Lawes, G
Goto, T
Tokura, Y
Ramirez, AP
机构
[1] Los Alamos Natl Lab, POB 1663, Los Alamos, NM 87545 USA
[2] Univ Tokyo, Dept Appl Phys, Tokyo 1138656, Japan
[3] ERATO, Japan Sci & Technol Agcy, Superstruct Project, Tsukuba, Ibaraki 3058562, Japan
[4] Bell Labs, Lucent Technol, Murray Hill, NJ 07974 USA
关键词
D O I
10.1103/PhysRevB.71.224425
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Magnetoelectric phase diagrams have been investigated for rare-earth manganites with orthorhombically distorted perovskite structure, RMnO3 (R=Gd, Tb, and Dy). A variety of magnetic and electric phases emerge with varying R-site ion, temperature, and magnetic field in these systems. The magnetoelectric phase diagram varies sensitively with the direction of a magnetic field relative to the crystallographic axes. Although the ground state of GdMnO3 with the largest ionic radius of R(r(R)) is not ferroelectric in zero magnetic fields (H=0), a ferroelectric phase with electric polarization (P) along the a axis appears by applying H(>similar to 1 T) along the b axis. Both TbMnO3 and DyMnO3 show a ferroelectric order with P along the c axis even at H=0 below a lock-in transition temperature where nonzero wave vectors for magnetic and lattice modulations become nearly constant. These systems also exhibit a flop of the ferroelectric polarization (P parallel to c to P parallel to a) when H is applied along the a or b axis. By contrast, the application of H above similar to 10 T along the c axis completely suppresses the ferroelectricity in TbMnO3. Possible origins of the observed evolution of magnetoelectric phases are discussed in consideration of magnetism and lattice distortion in the perovskite rare-earth manganites.
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