Trace Elements Distribution in the k7 Seam of the Karaganda Coal Basin, Kazakhstan

Aiman Kopobayeva, Irina Baidauletova, Altynay Amangeldikyzy, Nazym Askarova
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Abstract

We investigated the distribution patterns and evaluated the average contents of trace elements in the k7 seam of the Karaganda coal basin in Central Kazakhstan. This paper presents the results of studying the geochemistry of 34 elements in 85 samples of the k7 seam. The study employed a suite of advanced high-resolution analytical methods, including atomic emission spectrometry with inductively coupled plasma (ICP–OES) and mass spectrometry with inductively coupled plasma (ICP–MS), along with their processing and interpretation. It was determined that the concentrations of trace elements in the k7 seam are primarily associated with lithophile elements, revealing high concentrations of Li, V, Sc, Zr, Hf, and Ba. Additionally, increased concentrations of Nb, Ta, Se, Te, Ag, and Th were observed compared to the coal Clarke. Specific Nb(Ta)–Zr(Hf)–Li mineralization accompanied by a group of associated metals (Ba, V, Sc, etc.) was identified. The study revealed lateral and vertical heterogeneity of the rare elements’ distributions in coals, attributed to the formation dynamics of the coal basin. A correlation between Li and Al2O3 with a less positive relationship with K2O suggests the affinity of certain elements (Li, Ta, Nb, and Ba) to kaolinite. Clay layers showed increased radioactivity, with Th—13.2 ppm and U—2.6 ppm, indicating the possible presence of volcanogenic pyroclastic rocks characterized by radioactivity. Taken together, these data reveal the features of the rock composition of the source area, which is considered a mineralization source. According to geochemical data, it was found that the source area mainly consists of igneous felsic rocks, indicating that the formation occurred under conditions of a volcanic arc. This study’s novelty lies in estimating the average trace elements in the k7 seam, with elevated concentrations of certain elements that suggest promising prospects for industrial extraction from coals and coal wastes. These findings offer insights into considering coal as a potential source of raw material for rare metal production, guiding the industrial processing of key elements within coal. The potential extraction of metals from coal deposits, including from dumps, holds significance for industrial and commercial technologies, as processing critical coal elements can reduce disposal costs and mitigate their environmental impact.
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哈萨克斯坦卡拉干达煤盆地 k7 煤层中的微量元素分布
我们研究了哈萨克斯坦中部卡拉干达煤盆地 k7 煤层中微量元素的分布规律,并评估了其平均含量。本文介绍了对 k7 煤层 85 个样本中 34 种元素的地球化学研究结果。研究采用了一整套先进的高分辨率分析方法,包括电感耦合等离子体原子发射光谱法(ICP-OES)和电感耦合等离子体质谱法(ICP-MS),以及对这些方法的处理和解释。经测定,k7 煤层中的痕量元素浓度主要与亲岩元素有关,显示出 Li、V、Sc、Zr、Hf 和 Ba 的高浓度。此外,与 Clarke 煤层相比,Nb、Ta、Se、Te、Ag 和 Th 的浓度也有所增加。发现了特定的 Nb(Ta)-Zr(Hf)-Li 矿化,并伴有一组伴生金属(Ba、V、Sc 等)。研究揭示了煤中稀有元素分布的横向和纵向异质性,这归因于煤盆地的形成动力学。锂与 Al2O3 之间存在相关性,而与 K2O 之间的正相关性较小,这表明某些元素(锂、钽、铌和钡)与高岭石具有亲和性。粘土层显示出更高的放射性,钍含量为 13.2 ppm,铀含量为 2.6 ppm,表明可能存在以放射性为特征的火山成因火成碎屑岩。综合来看,这些数据揭示了被认为是矿化源的矿源区的岩石成分特征。根据地球化学数据,发现矿源区主要由火成岩长英岩组成,表明其形成是在火山弧条件下进行的。这项研究的新颖之处在于估算了 k7 煤层中的平均微量元素含量,其中某些元素的浓度较高,表明从煤炭和煤炭废料中进行工业提取的前景广阔。这些发现为将煤炭视为稀有金属生产的潜在原料来源提供了启示,指导了煤炭中关键元素的工业加工。从煤炭矿藏(包括垃圾场)中提取金属的可能性对工业和商业技术具有重要意义,因为对关键煤炭元素进行加工可以降低处理成本,减轻对环境的影响。
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