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Applied mineralogical characterization of ilmenite from Kahnuj placer deposit, Southern Iran

机译:伊朗南部卡努伊砂矿床中钛铁矿的应用矿物学表征

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Kahnuj placer deposit contains ilmenite and magnetite as the main valuable minerals. Microscopic and microprobe analyses show that ilmenite occurs in two forms as individual grains and exsolved lamellae within magnetite. Exsolved lamellae of hematite, sphene of different shape and rare rutile and zircon are found as inclusions in ilmenite. According to microprobe analysis data the TiO2 content of ilmenite (52.1 wt%) with small amounts of Mg and Mn and is very close to the theoretical one (52.6 wt%). Based on the XRF analysis, the maximum content of TiO2 in the purified ilmenite concentrate without any gangue minerals is obtained at 44 wt%. The low grade of TiO2 in the purified ilmenite is attributed to the presence of sphene and hematite inside ilmenite. The presence of sphene as a source of Ca and Si can negatively affect the quality of ilmenite concentrate and the further product titanium dioxide manufactured via chloride and sulphate routes. It is found that the magnetite from the deposit contains about 1.5 wt% of V2O3 and can be considered as important source for extraction of vanadium as a by-product.
机译:Kahnuj砂矿床含有钛铁矿和磁铁矿作为主要的有价值矿物。显微镜和探针分析表明,钛铁矿以两种形式存在,即单个晶粒和磁铁矿中溶解的薄片。在钛铁矿中发现了赤铁矿的溶解薄片,不同形状的细晶石和稀有的金红石和锆石。根据微探针分析数据,钛铁矿(52.1 wt%)中钛铁矿的含量为少量的Mg和Mn,非常接近理论值(52.6 wt%)。基于XRF分析,在没有任何脉石矿物的情况下,纯化的钛铁矿精矿中TiO 2的最大含量为44重量%。纯化钛铁矿中TiO2含量低的原因是钛铁矿内部存在和赤铁矿。 Sphene作为Ca和Si的来源会不利地影响钛铁矿精矿的质量以及通过氯化物和硫酸盐途径生产的其他产品二氧化钛。发现来自该沉积物的磁铁矿包含约1.5重量%的V 2 O 3,并且可以被认为是提取副产物钒的重要来源。

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