Vilarinho R, Weber M C, Guennou M, Miranda A C, Dias C, Tavares P, Kreisel J, Almeida A, Moreira J Agostinho
IFIMUP, Departamento de Física e Astronomia, Faculdade de Ciências, Universidade do Porto, rua do Campo Alegre s/n, 4169-007, Porto, Portugal.
Department of Materials, ETH Zurich, Vladimir-Prelog-Weg 4, 8093, Zurich, Switzerland.
Sci Rep. 2022 Jun 11;12(1):9697. doi: 10.1038/s41598-022-13097-1.
We investigate the interplay of magnetization and lattice vibrations in rare-earth orthoferrites RFeO, with a specific focus on non-symmetry-breaking anomalies. To do so, we study the magnetization, magnon excitations and lattice dynamics as a function of temperature in NdFeO, TbFeO, EuFeO and GdFeO. The magnetization shows distinct temperature anomalous behavior for all investigated rare-earth orthoferrites, even in the compounds with no phase transitions occurring at those temperatures. Through spin-phonon coupling, these magnetic changes are mirrored by the FeO rotation mode for all the studied RFeO, revealing a common magnetostructural effect associated with the octahedra rotations. The R oscillation modes evidence a Fe/R spins cross-talk for the NdFeO and TbFeO cases. Our work sheds light into the common magnetostructural coupling in rare-earth orthoferrites, and the important role of magnetic anisotropy and spin-orbit coupling strength of the R-Fe interactions on the spin-reorientation transition at high temperatures.
我们研究了稀土正铁氧体RFeO中磁化与晶格振动的相互作用,特别关注非对称性破缺异常。为此,我们研究了NdFeO、TbFeO、EuFeO和GdFeO中磁化、磁振子激发和晶格动力学随温度的变化。对于所有研究的稀土正铁氧体,即使在那些温度下没有发生相变的化合物中,磁化也表现出明显的温度异常行为。通过自旋-声子耦合,所有研究的RFeO的FeO旋转模式都反映了这些磁变化,揭示了与八面体旋转相关的共同磁结构效应。R振荡模式证明了NdFeO和TbFeO情况下Fe/R自旋的相互作用。我们的工作揭示了稀土正铁氧体中常见的磁结构耦合,以及R-Fe相互作用的磁各向异性和自旋-轨道耦合强度在高温自旋重取向转变中的重要作用。