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FeC/FeO核壳纳米颗粒中的交换偏置和韦尔维转变

Exchange bias and Verwey transition in FeC/FeO core/shell nanoparticles.

作者信息

Xing M, Mohapatra Jeotikanta, Elkins J, Guragain D, Mishra S R, Ping Liu J

机构信息

Department of Physics, The University of Texas at Arlington, Arlington, Texas 76019, USA.

Department of Physics and Materials Science, The University of Memphis, Memphis, TN 38152, USA.

出版信息

Nanoscale. 2021 Oct 1;13(37):15837-15843. doi: 10.1039/d1nr04520b.

Abstract

This report presents new findings of exchange bias and related structural and magnetic properties in iron carbide/magnetite (FeC/FeO) core/shell nanoparticles. The exchange bias emerges from an energetic landscape, namely a first-order phase transition-the Verwey transition at 125 K, during which the FeO shell changes from the cubic to monoclinic structure. The phase transition leads to the exchange bias because it results in abrupt changes in magnetocrystalline anisotropy and exchange coupling. Another unique phenomenon identified in this composite system is enhanced magnetic coercivity due to the uniaxial anisotropy of the monoclinic phase. An analysis of the correlations between the observed phenomena is given based on the temperature dependence of the coercivity, the exchange bias field values, and the Verwey transition temperature.

摘要

本报告介绍了碳化铁/磁铁矿(FeC/Fe₃O₄)核壳纳米颗粒中交换偏置以及相关结构和磁性的新发现。交换偏置源自一种能量景观,即一级相变——125K时的韦尔韦相变,在此期间Fe₃O₄壳层从立方结构转变为单斜结构。该相变导致交换偏置,因为它会引起磁晶各向异性和交换耦合的突然变化。在这个复合系统中发现的另一个独特现象是由于单斜相的单轴各向异性导致的矫顽力增强。基于矫顽力的温度依赖性、交换偏置场值和韦尔韦转变温度,对观察到的现象之间的相关性进行了分析。

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