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晶面和长径比对磁铁矿 FeO 纳米晶磁各向异性的作用。

The role of faceting and elongation on the magnetic anisotropy of magnetite FeO nanocrystals.

机构信息

Department of Physics, University of York, Heslington, York, YO10 5DD, UK.

Earth and Planetary Science, School of Geosciences, University of Edinburgh, Edinburgh, EH9 3FE, UK.

出版信息

Sci Rep. 2020 Feb 17;10(1):2722. doi: 10.1038/s41598-020-58976-7.

Abstract

FeO nanoparticles are one of the most promising candidates for biomedical applications such as magnetic hyperthermia and theranostics due to their bio-compatibility, structural stability and good magnetic properties. However, much is unknown about the nanoscale origins of the observed magnetic properties of particles due to the dominance of surface and finite size effects. Here we have developed an atomistic spin model of elongated magnetite nanocrystals to specifically address the role of faceting and elongation on the magnetic shape anisotropy. We find that for faceted particles simple analytical formulae overestimate the magnetic shape anisotropy and that the underlying cubic anisotropy makes a significant contribution to the energy barrier for moderately elongated particles. Our results enable a better estimation of the effective magnetic anisotropy of highly crystalline magnetite nanoparticles and is a step towards quantitative prediction of the heating effects of magnetic nanoparticles.

摘要

FeO 纳米颗粒由于其生物相容性、结构稳定性和良好的磁性能,是生物医学应用(如磁热疗和治疗诊断)中最有前途的候选材料之一。然而,由于表面和有限尺寸效应的主导地位,对于观察到的颗粒磁性的纳米级起源,我们知之甚少。在这里,我们开发了一种长形磁铁矿纳米晶体的原子自旋模型,专门研究晶面和伸长对磁形状各向异性的作用。我们发现,对于有晶面的颗粒,简单的解析公式高估了磁形状各向异性,而立方各向异性对中等伸长颗粒的能量势垒有重要贡献。我们的结果能够更好地估计高结晶磁铁矿纳米颗粒的有效磁各向异性,并朝着定量预测磁性纳米颗粒的加热效应迈出了一步。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b957/7026106/4e0f3a6ca9b1/41598_2020_58976_Fig1_HTML.jpg

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