Mineralogical and Structural Analyses of Natural Fluorite from Yantuwaru Mining Site, Nigeria

Gidado Shehu, Ibrahim Muhammad Bagudo
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引用次数: 1

Abstract

Experimental studies of natural fluorite have been reported. In this study, combined X-Ray Fluorescence, FTIR and UV-Vis analyses were performed to give mineralogical information about natural fluorspar. The X-ray diffraction technique was also used to determine the crystallographic parameters and structure of the mineral. Results show a variation of Ca contents and low concentration of F, through all fluorite samples due to Ba and Br contents in the samples, causing replacements of impurity ions in the fluorite lattice. REEs in the fluorite samples were to be found responsible for colour. UV-Visible absorption results showed peaks between 209 to 368 nm, which did not affect the fluorite colour. The 224 nm and 365 nm peaks were caused by the electrons and holes trapped in the Ca2+ interstitial and vacancy, respectively. The absorption bands in the visible range relate to the corresponding fluorite samples. The FTIR results showed absorptions causing CO2 and CO32-stretching vibration due to the CaCO3 and OH stretching vibration due to water in the samples. The structural configuration, the lattice parameters, and the planes confirmed a cubic structure. Obtained results confirmed them to be Calcium Fluorite, as expected.
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尼日利亚Yantuwaru矿区天然萤石的矿物学和结构分析
对天然萤石的实验研究已有报道。本文采用x射线荧光、红外光谱和紫外可见光谱相结合的方法对天然萤石进行了矿物学分析。x射线衍射技术还用于确定矿物的晶体学参数和结构。结果表明,由于样品中Ba和Br的含量,所有萤石样品中Ca含量发生了变化,F浓度较低,导致萤石晶格中杂质离子的替换。人们发现萤石样品中的稀土元素是造成颜色的原因。紫外可见吸收峰在209 ~ 368 nm之间,对萤石的颜色没有影响。224 nm和365 nm的峰分别是由Ca2+间隙和空位中捕获的电子和空穴引起的。在可见光范围内的吸收带与相应的萤石样品有关。FTIR结果表明,由于样品中CaCO3和OH的拉伸振动,吸收引起CO2和co32的拉伸振动。结构构型、晶格参数和面都确定了一个立方结构。所得结果证实其为萤石钙。
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