多铁BaTiO3、尖晶石MFe2O4 (M = Mn, Co, Ni, Zn)铁氧体和DMS ZnO纳米结构的铁磁性研究

K. Verma, Ashish Sharma, N. Goyal, R. Kotnala
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引用次数: 1

摘要

多铁性磁电材料对设计新型纳米级自旋电子器件具有重要意义。在单相多铁性batio3中,掺杂过渡金属TM离子,使其部分填满d轨道,从而产生磁性。有趣的是,磁有序与氧空位密切相关,因此,它被认为是TM: batio3铁磁性的来源。纳米结构的mfe2o4 (M = Mn, Co, Ni, Cu, Zn等)铁氧体具有反尖晶石结构,其中m2 +离子在八面体位上均匀分布,fe3 +离子在四面体和八面体位上均匀分布。这些反平行亚晶格(阳离子m2 +和fe3 +占据四面体或八面体位置)通过超交换作用与o2 -离子偶联形成铁磁结构。此外,未来自旋电子技术使用稀释磁性半导体,DMS材料可能已经实现铁磁性起源。在ZnO纳米粒子中同时掺杂TM和稀土离子,可以提高ZnO的反铁磁性有序度,从而获得高tc的铁磁性。在掺杂氧化锌中,氧空位作为主要缺陷的作用,必须涉及束缚磁极化子作为铁磁性的起源。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ferromagnetism in Multiferroic BaTiO3, Spinel MFe2O4 (M = Mn, Co, Ni, Zn) Ferrite and DMS ZnO Nanostructures
Multiferroic magnetoelectric material has significance for new design nanoscale spintronic devices. In single-phase multiferroic BaTiO 3 , the magnetism occurs with doping of transition metals, TM ions, which has partially filled d-orbitals. Interestingly, the magnetic ordering is strongly related with oxygen vacancies, and thus, it is thought to be a source of ferromagnetism of TM:BaTiO 3 . The nanostructural MFe 2 O 4 (M = Mn, Co, Ni, Cu, Zn, etc.) ferrite has an inverse spinel structure, for which M 2+ ions in octahedral site and Fe 3+ ions are equally distributed between tetrahedral and octahedral sites. These antiparallel sub-lattices (cations M 2+ and Fe 3+ occupy either tetrahedral or octahedral sites) are coupled with O 2- ion due to superexchange interaction to form ferrimagnetic structure. Moreover, the future spintronic technologies using diluted magnetic semiconductors, DMS materials might have realized ferromagnetic origin. A simultaneous doping from TM and rare earth ions in ZnO nanoparticles could increase the antiferromagnetic ordering to achieve high-Tc ferromagnetism. The role of the oxygen vacancies as the dominant defects in doped ZnO that must involve bound magnetic polarons as the origin of ferromagnetism.
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