南非林波波省Lwamondo和Zebediela Kaolins的起源和可能的应用

Pub Date : 2022-04-03 DOI:10.1080/25726838.2022.2063647
Avhatakali Raphalalani, G. Ekosse, J. Odiyo, J. Ogola, O. Oyebanjo, N. Bukalo
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引用次数: 1

摘要

摘要研究了南非Lwamondo和Zebediela高岭土的成因及其工业应用潜力。确定了选定的理化特性。采用XRD、SEM测定了矿物特征;用XRF和LA-ICP-MS测定其地球化学特征。高岭土的颜色通常是浅色(Lwamondo)和棕色(Zebediela)。两种高岭土均具有较低的pH(<6.5)和EC(<50µS/cm)。Lwamondo高岭土以壤土和粘壤土为主,而Zebediela高岭土以粘土、粉质和壤土为主。Lwamondo高岭土中主要矿物相为高岭石、蒙脱石和斜长石,Zebediela高岭土中主要矿物相为高岭石。高岭土的形态主要由高岭石片堆组成。高岭土的主要氧化物为SiO2、Al2O3和Fe2O3,轻稀土元素含量略有减少。研究结果表明:(1)高岭土形成于表生环境;(2)高岭土适合制作空心砖。
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Genesis and possible applications of Lwamondo and Zebediela Kaolins, Limpopo Province, South Africa
ABSTRACT The genesis and potential industrial applications of Lwamondo and Zebediela Kaolins in South Africa were determined. Selected physico-chemical characteristics were determined. Mineralogical characteristics were determined using XRD and SEM; and geochemical characteristics were determined using XRF and LA-ICP-MS. Kaolin colours were generally light (Lwamondo) and brown (Zebediela). Both kaolins had low pH (<6.5) and EC (<50 µS/cm). The texture of Lwamondo Kaolin was generally loam and clay loam, whereas that of Zebediela was clayey, silty and loamy. Major mineral phases were kaolinite, smectite and plagioclase in Lwamondo Kaolin, and kaolinite in Zebediela Kaolin. The morphology of the kaolins consisted mainly of stacks of kaolinite flakes. The most dominant major oxides were SiO2, Al2O3 and Fe2O3, and the kaolins were slightly depleted in light rare earth elements. The studied characteristics indicated that the kaolins (i) formed in a supergene environment and (ii) are suitable for hollow bricks.
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