Structure and magnetic properties of magnesium ferrite fine powders

S.A. Oliver, R.J. Willey, H.H. Hamdeh, G. Oliveri, G. Busca
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引用次数: 49

Abstract

Fine powders of magnesium ferrite, MgFe2O4, were produced through the sol-gel supercritical drying method, with two portions then being calcined at 773 K and 1073 K. The powder structural and magnetic properties were determined from transmission electron microscope micrographs, x-ray diffraction, Mössbauer effect spectroscopy and magnetometry measurements. The powder structure matched the MgFe2O4 spinel phase, with small amounts of α-Fe2O3 being observed in heated samples. As-produced powders were superparamagnetic at room temperature, with single magnetic domain particle behavior being observed at low temperatures, and for the 1073 K heated sample. The particle size distribution for the as-produced powder was evaluated separately from the micrographs, by fitting the magnetization data to a weighted Langevin function, and by fitting Mössbauer spectra taken at temperatures from 25 K to 298 K. Very similar particle size distributions were found from all three methods. The average particle diameter was 11 nm for the as-produced powder, and increased for heated samples. The saturation magnetization and magnetocrystalline anisotropy energy density values were both consistent with bulk values, in contrast to the large differences between particle and bulk values described for other fine particle systems.

铁氧体镁细粉的结构与磁性能
采用溶胶-凝胶超临界干燥法制备铁酸镁(MgFe2O4)细粉,分别在773 K和1073 K下煅烧。通过透射电子显微镜、x射线衍射、Mössbauer效应光谱和磁强计测定了粉末的结构和磁性能。粉末结构与MgFe2O4尖晶石相相一致,加热后样品中存在少量α-Fe2O3。制备的粉末在室温下具有超顺磁性,在低温和1073 K加热样品中观察到单磁畴颗粒行为。通过将磁化数据拟合到加权朗之万函数,并通过拟合温度从25 K到298 K的Mössbauer光谱,分别从显微照片中评估了生产粉末的粒度分布。从这三种方法中发现非常相似的粒度分布。制备的粉末的平均粒径为11 nm,加热后的样品粒径增大。饱和磁化强度和磁晶各向异性能量密度值与体体值一致,而其他细颗粒体系的颗粒值与体体值存在较大差异。
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