Extraction of Alumina from Kaolin found in Gem Mining Sites of Sri Lanka

Y. D. T. I. Karunarathna, R. C. L. D. Silva
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Abstract

Kaolinitic clay deposits, esteemed as valuable mineral resources in Sri Lanka, are widely distributed throughout the country. Clay deposits in the Ratnapura District are often unearthed during gem mining operations. Unfortunately, excavated deposits are frequently disposed of openly on the ground without undergoing any value-addition process. This practice alters the soil condition of the vicinity, as the clay soil blocks the gravitational flow of rainwater. This environmental impact can be overcome by adding commercial value to these kaolinitic clay deposits. The present study aims to demonstrate the feasibility of extracting alumina from kaolinitic clay found at gem mining sites and to evaluate the potential of the extracted alumina as an adsorbent. Kaolinitic clay samples were collected from a gem mining site in the Ratnapura District. First, kaolin was transformed into metakaolin through calcination, and then alumina was extracted from the metakaolin via acid leaching using HCl as the leaching agent. Aluminum ions were separated from the leaching solution as Al(OH)₃ using NaOH as the precipitant. The precipitated Al(OH)₃ was transformed into alumina by calcination. The adsorption properties of the extracted alumina were evaluated using methylene blue solution as the adsorbate. Kaolin, extracted, and commercial alumina samples were characterized using XRD, XRF, FTIR, and SEM analysis. XRF analysis revealed that kaolin consists of 29.11 % alumina by weight, and the purity of the extracted alumina was 90.03%. The crystalline phase of extracted alumina was identified as the γ phase via XRD analysis. Extracted and commercial alumina exhibited similar trends in the adsorption of methylene blue under varying adsorption parameters. Accordingly, γ-phase alumina with a purity exceeding 90% can be produced from the kaolinitic clay found at the gem mining site under these experimental conditions. The extracted alumina has demonstrated potential for use as an adsorbent, exhibiting compatibility with commercial alumina.
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从斯里兰卡宝石开采地发现的高岭土中提取氧化铝
高岭土粘土矿床是斯里兰卡宝贵的矿产资源,广泛分布于全国各地。拉特纳普勒地区的粘土矿藏往往是在宝石开采过程中出土的。遗憾的是,挖掘出的矿藏往往未经任何增值处理就被随意丢弃在地面上。这种做法会改变附近的土壤条件,因为粘土会阻碍雨水的重力流动。通过增加这些高岭土沉积物的商业价值,可以克服这种环境影响。本研究旨在证明从宝石开采地发现的高岭土中提取氧化铝的可行性,并评估提取的氧化铝作为吸附剂的潜力。高岭土样本采集自 Ratnapura 地区的一个宝石开采点。首先,通过煅烧将高岭土转化为偏高岭土,然后使用盐酸作为浸出剂,通过酸浸法从偏高岭土中提取氧化铝。以 NaOH 为沉淀剂,铝离子以 Al(OH)₃ 的形式从浸出液中分离出来。沉淀的 Al(OH)₃ 通过煅烧转化为氧化铝。以亚甲基蓝溶液为吸附剂,对提取的氧化铝的吸附特性进行了评估。利用 XRD、XRF、FTIR 和 SEM 分析对高岭土、提取物和商用氧化铝样品进行了表征。XRF 分析表明,按重量计,高岭土含有 29.11% 的氧化铝,提取的氧化铝纯度为 90.03%。通过 XRD 分析,确定提取的氧化铝的结晶相为 γ 相。在不同的吸附参数下,提取的氧化铝和商用氧化铝对亚甲基蓝的吸附趋势相似。因此,在这些实验条件下,可以从宝石开采地发现的高岭土中生产出纯度超过 90% 的 γ 相氧化铝。提取的氧化铝具有用作吸附剂的潜力,与商用氧化铝兼容。
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