坦桑尼亚西南部njombe地区Matamba高岭土矿床的矿物学和地球化学特征:对工业应用的影响

Melania A. Nyimbo, Ronald J. Massawe, Michael M. Msabi
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摘要

高岭土是一种商业粘土材料,由水合铝硅酸盐矿物高岭石组成,用于各种工业应用,如陶瓷,造纸,油漆,耐火材料,玻璃纤维,塑料,化妆品和制药。它是在较低的温度和压力条件下结晶和富长石岩石的强烈化学风化作用或花岗质岩石的热液蚀变作用的结果。马坦巴高岭土矿床起源于非洲陆面发育过程中白长辉长岩的风化作用。鉴于马坦巴高岭土的突出性质,对其矿物学和化学特征进行了研究,以确定其工业应用价值。作为研究方法的一部分,收集了46(46)个样品,并使用x射线荧光(XRF)和x射线衍射(XRD)分析了主要氧化物。XRD结果表明,Matamba高岭土主要由高岭石(10.1 ~ 100%)组成,其他相为钠长石(1.2 ~ 56.8%)、低晶长石(10.1 ~ 54.3%)、石英(1.2 ~ 33.9%)、针铁矿(1.0 ~ 9.4%)和白云母(1.1 ~ 29.5%)。主要氧化物为SiO2 (39.78 ~ 67.96 wt.%)、Al2O3 (14.60 ~ 38.07 wt.%),其次为Fe2O3 (0.93 ~ 6.37 wt.%)、MgO (1.42 ~ 4.74 wt.%)、Na2O (0.10 ~ 1.09 wt.%)、K2O (0.14 ~ 2.01 wt.%)、CaO (0.08 ~ 0.99 wt.%)、TiO2 (0.07 ~ 1.66 wt.%)、P2O5 (0.36 ~ 1.77 wt.%)和LOI (1.91 ~ 13.97 wt.%)。这些主要的氧化物与支持高岭石优势的矿物组成有关。因此,与一些工业规格相比,这些结果表明,马坦巴高岭土矿床可用于陶瓷产品,耐火材料,如耐火粘土坩埚和铝及其合金的电解生产。然而,它应该被选矿和升级,以提高一些技术性能,以符合其他工业应用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mineralogy and Geochemical Characteristics of Matamba Kaolin Deposit-Njombe Region South-Western Tanzania: Implications for Industrial Applications
Kaolin is a commercial clay material composed of hydrated aluminosilicate mineral kaolinite and used in various industrial applications such as ceramics, paper, paints, refractories, fiberglass, plastics, cosmetics and pharmaceuticals. It is formed as a result of strong chemical weathering of crystalline and feldspar-rich rocks or hydrothermal alteration of granitic rocks at relatively low temperature and pressure conditions. The kaolin deposit of Matamba originated from the weathering of leucogabbro rock during the development of the African land surface. In view of highlighted properties, the mineralogy and chemical characteristics of the Matamba kaolin deposit were investigated to determine its industrial applications. As part of the study approach, forty-six (46) samples were collected and analyzed for major oxides using X-ray fluorescence (XRF) and mineralogical composition using X-ray diffraction (XRD). The XRD results indicated that the Matamba kaolin is dominantly composed of kaolinite (10.1–100%) with other phases such as albite (1.2–56.8%), oligoclase (10.1–54.3%), quartz (1.2–33.9%), goethite (1.0–9.4%) and muscovite (1.1–29.5%). The dominant major oxides are SiO2 (39.78–67.96 wt.%), Al2O3 (14.60–38.07 wt.%) and subordinate amounts of Fe2O3 (0.93–6.37 wt.%), MgO (1.42–4.74 wt.%), Na2O (0.10–1.09 wt.%), K2O (0.14–2.01 wt.%), CaO (0.08–0.99 wt.%), TiO2 (0.07–1.66 wt.%), P2O5 (0.36–1.77 wt.%) and LOI (1.91–13.97 wt.%). These major oxides correlate with the mineralogical composition supporting kaolinite dominance. Consequently, compared with some industrial specifications, these results indicate that Matamba kaolin deposit may be useful for ceramic products, refractories such as fireclay crucibles and electrolytic production of aluminium and its alloys. However, it should be beneficiated and upgraded to improve some technical properties to qualify for other industrial applications.
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