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Existence Of Fe~(4+)Ions In Co_(2.25)Fe_(0.75)O_4 Spinel Ferrite Confirmed From SXRD And XANES Spectroscopy

机译:来自SXRD和XANES光谱的CO_(2.25)FE_(0.75)O_4尖晶石铁氧体的FE〜(4+)离子的存在性

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摘要

The Co_(2.25)Fe_(0.75)O_4 ferrite composition has been prepared by chemical co-precipitation route. The as-prepared sample after annealing at 900 °C in air formed single phase cubic spinel structure. Synchrotron X-ray diffraction and X-ray absorption near edge structure (XANES) measurements were used to study charge states of the cations in octahedral and tetrahedral sites of the cubic spinel structure. Raman spectra indicated normal cubic spinel structure. XANES data suggested the existence of Fe~(4+) ions in the spinel structure.
机译:CO_(2.25)Fe_(0.75)O_4铁氧体组合物由化学共沉淀途径制备。在空气中在900℃下退火后的AS制备的样品形成单相立方尖晶石结构。边缘结构(XANES)测量附近的同步X射线衍射和X射线吸收用于研究立方尖晶石结构的八面体和四面体位点的阳离子的电荷状态。拉曼光谱表示正常立方尖晶石结构。 XANES数据表明尖晶石结构中Fe〜(4+)离子的存在。

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