单相磁赤铁矿(γ-Fe2O3)纳米晶粉体的结构和磁性能

J. A. R. Guivar, Arturo I. Martínez, A. O. Anaya, L. Valladares, L. L. Félix, A. Domínguez
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引用次数: 61

摘要

本文报道了用化学共沉淀法合成的单相磁赤铁矿(γ-Fe2O3)磁性纳米晶(MNCs)的结构和磁性研究。在不含表面活性剂的酸性介质中,在80℃下调节pH = 3.5,在室温下氧化碱性介质中磁铁矿(Fe3O4)的起始前驱体。x射线衍射(XRD)图显示宽峰表明纳米尺寸,Rietveld细化证实只有一个单相分配给γ-Fe2O3跨国公司。高分辨率透射电子显微镜(HR-TEM)显示形成的纳米颗粒直径约为D≈6.8±0.1 nm,与Rietveld细化(6.4±1 nm)一致。选择了一个区域的电子衍射图来补充对γ-Fe2O3 MNCs晶体结构的研究。在不同温度下进行的M(H)测量显示矫顽力和剩余力几乎为零,表明超顺磁畴和高磁饱和度。
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Structural and Magnetic Properties of Monophasic Maghemite (γ-Fe2O3) Nanocrystalline Powder
Structural and magnetic studies of monophasic maghemite (γ-Fe2O3) magnetic nanocrystallites (MNCs) synthesized by the co-precipitation chemical route are reported in this paper. For the synthesis, a starting precursor of magnetite (Fe3O4) in basic medium was oxidized at room temperature by adjusting the pH = 3.5 at 80°C in an acidic medium without surfactants. X-ray diffraction (XRD) pattern shows widened peaks indicating nanometric size and Rietveld Refinement confirms only one single-phase assigned to γ-Fe2O3 MNCs. High Resolution Transmission Electron Microscopy (HR-TEM) demonstrates the formation of nanoparticles with diameter around D ≈ 6.8 ± 0.1 nm which is in good agreement with Rietveld Refinement (6.4 ± 1 nm). A selected area electron diffraction pattern was carried out to complement the study of the crystalline structure of the γ-Fe2O3 MNCs. M(H) measurements taken at different temperatures show almost zero coercivity and remanence indicating superparamagnetic domain and high magnetic saturation.
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