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.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据