Chemometric quantification of trace element impurities within kaolin and talc white clay minerals in Kutch and Banas-Mahi basin, India

IF 1.827 Q2 Earth and Planetary Sciences
Prashant Shriram Wagh, Ravishankar Kumar, Sanjeev Bhasin, Pawan Pal
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引用次数: 0

Abstract

The unique properties of kaolin-talc white clays such as hydration, plasticity, rheological, color, and adsorption capacities are affected by the existence of elemental/trace metal impurities. A systematic and comprehensive study regarding elemental/trace metal impurities in kaolin and talc is lacking. Thus, the present study investigated elemental impurities in kaolin and talc and their source apportionment pattern. For this concern, a total of 50 kaolin samples from the Bhuj area of the Kutch basin (Gujarat, India) and 30 talc samples from the Mahi-Banas basin of Rajasthan (Bhilwara, Udaipur, and Dungarpur) were analyzed. The major trace element impurities such as lead (Pb), chromium (Cr), copper (Cu), nickel (Ni), arsenic (As), manganese (Mn), and zinc (Zn) were detected in kaolin-talc clays from inductively coupled plasma optical emission spectrometry (ICP-OES) technique. Further, the source apportionment study was carried out by using multivariate analyses such as principal component analysis (PCA), hierarchical cluster analysis (HCA), and Pearson correlation matrix (PCM). The results indicated that the mean concentrations of trace elements Cr, Pb, Mn, Ni, Zn, Cu, and As in kaolin were 114, 57.82, 33.31, 20.36, 16.51, 10.98, and 0.05 mg/kg, respectively, whereas 2.53, 0.63, 159, 5.05, 20.11, 1.22, and 11.23 mg/kg, correspondingly, in talc samples. However, the toxic elemental impurity level was low as compared to Indian and European Union standards for soils. The present study explores the existence of major trace elemental impurities in kaolin-talc clays. Furthermore, the multivariate analyses described that the major sources of existing elemental impurities are attributed as being from different geogenic sources.

印度Kutch和Banas-Mahi盆地高岭土和滑石白色粘土矿物中微量元素杂质的化学计量定量
高岭土-滑石白粘土的水化、塑性、流变性、颜色和吸附能力等独特性能受到元素/微量金属杂质存在的影响。目前对高岭土和滑石中的元素/微量金属杂质缺乏系统、全面的研究。因此,本研究探讨了高岭土和滑石中的元素杂质及其来源分配模式。为此,研究人员对来自印度古吉拉特邦Kutch盆地Bhuj地区的50个高岭土样本和来自拉贾斯坦邦Mahi-Banas盆地(bilwara、Udaipur和Dungarpur)的30个滑石样本进行了分析。采用电感耦合等离子体发射光谱法(ICP-OES)测定了高岭土中铅(Pb)、铬(Cr)、铜(Cu)、镍(Ni)、砷(as)、锰(Mn)、锌(Zn)等主要微量元素杂质。进一步,通过主成分分析(PCA)、层次聚类分析(HCA)和Pearson相关矩阵(PCM)等多变量分析进行源分配研究。结果表明,高岭土样品中微量元素Cr、Pb、Mn、Ni、Zn、Cu和As的平均浓度分别为114、57.82、33.31、20.36、16.51、10.98和0.05 mg/kg,滑石样品中微量元素Cr、Pb、Mn、Ni、Zn、Cu和As的平均浓度分别为2.53、0.63、159、5.05、20.11、1.22和11.23 mg/kg。然而,与印度和欧盟的土壤标准相比,有毒元素杂质水平较低。本研究探讨了高岭土-滑石粘土中主要微量元素杂质的存在。此外,多变量分析表明,现有元素杂质的主要来源归因于不同的地质来源。
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来源期刊
Arabian Journal of Geosciences
Arabian Journal of Geosciences GEOSCIENCES, MULTIDISCIPLINARY-
自引率
0.00%
发文量
1587
审稿时长
6.7 months
期刊介绍: The Arabian Journal of Geosciences is the official journal of the Saudi Society for Geosciences and publishes peer-reviewed original and review articles on the entire range of Earth Science themes, focused on, but not limited to, those that have regional significance to the Middle East and the Euro-Mediterranean Zone. Key topics therefore include; geology, hydrogeology, earth system science, petroleum sciences, geophysics, seismology and crustal structures, tectonics, sedimentology, palaeontology, metamorphic and igneous petrology, natural hazards, environmental sciences and sustainable development, geoarchaeology, geomorphology, paleo-environment studies, oceanography, atmospheric sciences, GIS and remote sensing, geodesy, mineralogy, volcanology, geochemistry and metallogenesis.
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