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首页> 外文期刊>Journal of Material Sciences & Engineering >Application of Gettering Process on the Improvement of the Structural and Mineralogical Properties of Tunisian Phosphate Rock
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Application of Gettering Process on the Improvement of the Structural and Mineralogical Properties of Tunisian Phosphate Rock

机译:吸气工艺在改善突尼斯磷矿结构和矿物学特性中的应用

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The present study deals with the effects of gettering process on the structural and mineralogical composition of Tunisian phosphate rock. The treated samples were characterized to investigate the variation of physical structure and chemical composition as compared to the reference phosphate rock. The quantitative analysis of the impurities concentration before and after gettering treatment using energy-dispersive (EDX) reveals a significant reduction of impurity concentration (more than 75%) such as Al, Si, S, Na, and Mg. Scanning electron microscopy (SEM) shows that gettering process promoted structural alterations of phosphate rock sample due to fusion of impurities. The XRD patterns show that the chief mineral constituent of treated sample is only fluorapatite, while those in the reference ore were calcite, dolomite, quartz and carbonate-fluorapatite. FT-IR characterization show a disappearance of the bands related to calcite at 714 cm-1 as well as B carbonate situated at 1430 cm-1, 1458 cm-1 after gettering treatment. This result is in good correlation with Raman analysis.
机译:本研究涉及吸气过程对突尼斯磷矿结构和矿物组成的影响。对处理后的样品进行表征以研究与参考磷酸盐岩相比的物理结构和化学组成的变化。使用能量分散(EDX)进行的吸杂处理前后的杂质浓度定量分析显示,Al,Si,S,Na和Mg等杂质浓度显着降低(超过75%)。扫描电子显微镜(SEM)表明,由于杂质的融合,吸杂过程促进了磷酸盐岩样品的结构改变。 X射线衍射图谱表明,处理后的样品的主要矿物成分仅为氟磷灰石,而参考矿石中的主要矿物成分为方解石,白云石,石英和碳酸盐-氟磷灰石。 FT-IR表征显示,吸杂处理后,与方解石相关的谱带在714 cm-1处消失,碳酸盐B碳在1430 cm-1、1458 cm-1处消失。该结果与拉曼分析具有良好的相关性。

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