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Magnetoelectric properties of epitaxial ferrite garnet films

机译:外延铁氧体石榴石薄膜的磁电性能

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摘要

Magnetoelectric properties of ferrite garnets are of great interest due to possibility of electric control of micromagnetic structures at room temperatures promising for applications in advanced technologies. However, the governing mechanisms underlying magnetoelectric coupling and origin of ferroelectricity in these materials remain under discussion. In this article, we appeal to polar mechanism related to electric dipole moments of Fe3+ and rare earth ions in order to explain ferroelectricity of epitaxial ferrite garnet film. We show that existence of electric dipole moments of 'd' (Fe3+) ions and 'f' (rare earth) ions is allowed by the local symmetry of the environments and calculate electric polarization related to electric dipole moments of the 'd' and the 'f' ions in inhomogeneously magnetized ferrite garnet film. Our results suggest that magnetoelectricity of iron garnets is attributed to polarizability of Fe3+ and rare earth ions; the conducted calculations demonstrate the difference between polarization impacts given by electric dipole moments of rare earth and iron ions. Polarization depend on ground state of the ions, local symmetry of the ions environments and the type of magnetic inhomogeneity. (C) 2018 Elsevier B.V. All rights reserved.
机译:铁氧体石榴石的磁电特性引起人们极大的兴趣,这是因为有可能在室温下对微磁结构进行电控制,有望应用于先进技术中。但是,这些材料中的磁电耦合和铁电起源的控制机理仍在讨论中。在本文中,我们呼吁与Fe3 +和稀土离子的电偶极矩有关的极性机制,以便解释外延铁氧体石榴石薄膜的铁电性。我们证明环境的局部对称性允许存在'd'(Fe3 +)离子和'f'(稀土)离子的电偶极矩,并计算与'd'和(d3)的电偶极矩有关的电极化。非均匀磁化的铁氧体石榴石薄膜中的“ f”离子。我们的研究结果表明,铁石榴石的磁电性归因于Fe3 +和稀土离子的极化性。进行的计算证明了稀土和铁离子的电偶极矩所产生的极化影响之间的差异。极化取决于离子的基态,离子环境的局部对称性以及磁不均匀性的类型。 (C)2018 Elsevier B.V.保留所有权利。

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