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Structural, Spectroscopic, Magnetic, and Thermal Characterizations of a Magnetite Ore from the Nagaland Region, India

机译:来自印度纳卡兰地区的磁铁矿矿石的结构,光谱,磁性和热特征

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An Indian magnetite ore from the Nagaland region was characterized by powder X-ray diffraction, spectroscopies (ultraviolet-visible and Raman), high temperature magnetization and thermal analysis. A Rietveld refinement of the diffraction data revealed that the principal phase present in the sample is magnetite with partial substitution of Fe with Mg (mainly) and Cr, leading to the chemical formula of MgCr_(0.2)Fe_(1.8)O_4. The UV-visible spectra of the sample in MeCN solution showed three distinct peaks. The lower region bands are due to metal-oxygen charge transitions and the other band is for d-d transition of iron. Raman spectral study at room temperature gave four characteristics bands of magnetite. The sample underwent a magnetic transition at high temperature and the thermomagnetization curve shows hysteresis during cooling cycle which indicates the possibility of first order structural transition at high temperature. The thermal property of the concentrate was studied by differential scanning calorimetric technique.
机译:来自纳加兰地区的印度磁铁矿矿石的特征在于粉末X射线衍射,光谱(紫外 - 可见和拉曼),高温磁化和热分析。衍射数据的RIETVELD细化显示,样品中存在的主要相是磁铁矿,其具有Mg(主要)和Cr的部分取代Fe,导致MgCR_(0.2)Fe_(1.8)O_4的化学式。 MECN溶液中样品的UV可见光光谱显示出三个不同的峰。下部区域带是由于金属 - 氧电荷转变,另一个带是铁的D-D转变。室温下拉曼光谱研究得到了四个特征磁铁矿。样品在高温下接受磁性转变,并且热磁化曲线在冷却循环期间显示滞后,这表明在高温下的第一阶结构转变的可能性。通过差示扫描量热技术研究了浓缩物的热性。

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