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La2O3FeMnSe2 的磁性结构:中子衍射和物理性质测量。

Magnetic structure of La2O3FeMnSe2: neutron diffraction and physical property measurements.

机构信息

Helmholtz Zentrum Berlin, Hahn-Meitner Platz 1, D-14109 Berlin, Germany.

出版信息

J Phys Condens Matter. 2013 Feb 27;25(8):086004. doi: 10.1088/0953-8984/25/8/086004. Epub 2013 Jan 31.

Abstract

We report on the characterization of the mixed layered lanthanum iron manganese oxyselenide La(2)O(3)FeMnSe(2), where Fe and Mn share the same crystallographic position. The susceptibility data show a magnetic transition temperature of 76 K and a strong difference between field cooled and zero field cooled (ZFC) data at low fields. While the ZFC magnetization curve exhibits negative values below about 45 K, hysteresis measurement reveals, after an initial negative magnetic moment, a hysteresis loop typical for ferromagnetic material, pointing to competing ferromagnetic and antiferromagnetic interactions. Resistivity and dielectric permittivity measurements indicate that La(2)O(3)FeMnSe(2) is a semiconductor. We performed x-ray diffraction at 295 K and neutron diffraction at 90 and 1.7 K. The nuclear and magnetic structure was refined in the space group I4/mmm with a = 4.11031 (3) Å and c = 18.7613 (2) Å at 295 K. We did not detect a structural distortion and the Fe and Mn atoms were randomly distributed. The magnetic order was found to be antiferromagnetic, with a propagation vector q = (0,0,0) and magnetic moments of 3.44 (5) μ(B) per Fe/Mn atom aligned within the a-b plane. This magnetic order is different with respect to the pure Fe or Mn compositions reported in other studies.

摘要

我们报告了混合层镧铁锰氧硒化物 La(2)O(3)FeMnSe(2)的特性,其中 Fe 和 Mn 占据相同的晶体位置。磁化率数据显示,磁转变温度为 76 K,在低场下,磁场冷却和零场冷却(ZFC)数据之间存在很大差异。虽然 ZFC 磁化曲线在约 45 K 以下呈现负值,但磁滞测量显示,在初始负磁矩之后,呈现出铁磁材料的典型磁滞回线,表明存在竞争的铁磁和反铁磁相互作用。电阻率和介电常数测量表明 La(2)O(3)FeMnSe(2)是一种半导体。我们在 295 K 进行了 X 射线衍射,在 90 和 1.7 K 进行了中子衍射。在 295 K 时,核和磁结构在空间群 I4/mmm 中进行了精修,a = 4.11031(3)Å,c = 18.7613(2)Å。我们没有检测到结构变形,Fe 和 Mn 原子随机分布。发现磁有序为反铁磁,传播矢量 q = (0,0,0),每个 Fe/Mn 原子的磁矩为 3.44(5)μB,在 a-b 平面内排列。这种磁有序与其他研究中报道的纯 Fe 或 Mn 组成不同。

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