Probing of order parameters in magnetoelectric multiferroics by neutron diffraction

K. Krezhov
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Abstract

Neutron scattering methods are indispensable in studying structure-property relationships. Determination of spin arrangements in magnetically ordered materials makes neutron diffraction among the major tools in the research on multiferroics because to understand why a given compound displays or does not display the expected properties calls for detailed information on microscopic level. We describe the efforts to identify new candidate magnetoelectric materials based primarily on considerations of symmetry and the knowledge of the magnetic structure. We found that substitution of half manganese with iron introduces a low level of disorder between the two transition metal positions in the RFeMnO5 (R=Tb,Yb) structure. The lack of evidence for a crystallographic phase transition to a polar space group rules out expectations of a spontaneous electric polarization. In addition, the observed collinear magnetic structure with k = 0 does not permit a spin polarization.. Therefore, by contrast to well known multiferroics RMn2O5 (R=Tb,Yb), YbMnFeO5 and TbMnFeO5 is not expected to be multiferroic compounds. Other examples in this article include nanosize powder material from the mixed oxide system YFexCr1−xO3 and Y-type hexaferrite multiferroic Ba2Mg2Fe12O22 as well as antiferromagnetic La0.5Pb0.5FeO3.
用中子衍射探测磁电多铁体的有序参数
中子散射方法是研究结构-性质关系不可缺少的方法。确定磁有序材料中的自旋排列使中子衍射成为研究多铁性的主要工具之一,因为要理解为什么给定的化合物显示或不显示预期的性质需要在微观水平上的详细信息。我们描述的努力,以确定新的候选磁电材料主要基于对称性的考虑和磁性结构的知识。我们发现用铁取代一半锰在RFeMnO5 (R=Tb,Yb)结构的两个过渡金属位置之间引入了低水平的无序。缺乏晶体相变到极空间群的证据排除了自发电极化的期望。此外,当k = 0时,观察到的共线磁结构不允许自旋极化。因此,与已知的多铁化合物RMn2O5 (R=Tb,Yb)相比,YbMnFeO5和TbMnFeO5不被认为是多铁化合物。本文中的其他例子包括来自混合氧化物体系YFexCr1−xO3和y型六铁体多铁性Ba2Mg2Fe12O22的纳米级粉末材料以及反铁磁性La0.5Pb0.5FeO3。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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