T. Koutzarova, S. Kolev, K. Krezhov, B. Georgieva, C. Ghelev, Todor Cholakov, L. Tran, M. Babij
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引用次数: 0
摘要
多铁氧体材料是一类特殊的磁性材料,其中长程磁序和铁电序共存,因此从基础和实用角度都引起了研究人员的兴趣。磁电多铁氧体是结合了耦合电偶极子和磁偶极子的材料。最近,研究的重点是一些六方铁氧体中磁电效应的发生,以及将其用作单相多铁氧体和磁电材料的可能性。多年来,人们对各种六方铁氧体作为永磁体、高密度记录介质、微波器件、生物医学应用等材料进行了深入研究。事实证明,磁性结构,特别是特定条件下的磁自旋排列,是实现六元晶磁电相的关键因素。在此,我们将概述最近在研究 Y 型六铁氧体磁性相变方面取得的一些进展。特别是以 Ba0.5Sr1.5Zn2Fe12O22 为例,说明了用磁性阳离子取代非磁性 Me2+ 阳离子和用非磁性阳离子取代磁性 Fe3+ 阳离子对 Y 型六价铁磁体的磁性能和磁相变的影响。
HEXAFERRITES - SINGLE PHASE MAGNETO-ELECTRIC MULTIFERROICS
Multiferroic materials are an exceptional class of magnetic materials where long-range magnetic and ferroelectric orders coexist, thus provoking the researchers’ interest from both basic and practical points of view. The magneto-electric multiferroics are materials that combine coupled electric and magnetic dipoles. Recently, research has focused on the occurrence of the magnetoelectric effect in some hexagonal ferrite types and the possibility of their use as single-phase multiferroic and magnetoelectric materials. For many years, various hexaferrites have been intensively studied as materials for permanent magnets, high-density recording media, microwave devices, biomedical applications, etc. The magnetic structure and especially the specific magnetic spin arrangement under certain conditions proved to be key factors for the realization of magneto-electric phases in hexaferrites. Here some recent advances in our studies of the magnetic phase transitions in the Y-type hexaferrites are overviewed. In particular, the influence of the replacement of non-magnetic Me2+ cations with magnetic cations and of magnetic Fe3+ cations with non-magnetic ones on the magnetic properties and occurring magnetic phase transitions in Y-type hexaferrites are exemplified with Ba0.5Sr1.5Zn2Fe12O22.