Mineralogical and elemental analysis of Kazakh coals from three mines: Preliminary insights from mode of occurrence to environmental impacts

dc.contributor.authorMedet Junussov
dc.contributor.authorFarkhad Tarikhov
dc.contributor.authorAbaidildin Abildakhanov
dc.contributor.authorDauren Zhanaidar
dc.contributor.authorGulnur Mekenbek
dc.contributor.authorAizada Assambayeva
dc.date.accessioned2025-08-26T11:27:16Z
dc.date.available2025-08-26T11:27:16Z
dc.date.issued2024-01-01
dc.description.abstractThis study aims to comprehensively characterize coal extracted from three active mines in northeastern Kazakhstan: Lenin, Saradyr, and Bogatyr. These mines exploit two Carboniferous coal-bearing formations, Dolyn and Karagandy. Dolyn, extracted by the Lenin underground mine at a depth of 700 m, contrasts with Karagandy, extracted at depths up to 260 m in Saradyr and Bogatyr. Six selected samples from the Lenin, Saradyr, and Bogatyr mines underwent various analyses, including proximate and ultimate analyses, elemental analyses (acid digestions with HCl + HNO 3 + HF, ICP-MS), and determination of mineral matter contents (XRD and SEM-EDS). This research aimed to understand the mode of occurrence of minerals and elements, technological and environmental implications of the coal seams extracted from these mines. Results indicate low sulfur and high ash content in the organic matter of all samples. Quartz and kaolinite dominate, with minor euhedral pyrite present in all samples. Framboidal pyrite, iron oxides, and rare earth element (REE)-bearing minerals are exclusively found in Saradyr and Bogatyr samples. Quartz and kaolinite likely reached the peat swamp through detrital processes, while pyrite formation occurred through both syngenetic and epigenetic processes in the coal samples. Ratios like Ce n /Ce n , Eu n /Eu n , Y n /Ho n , and Gd n /Gd n suggest REE deposition in anoxic hydrothermal water environments, possibly indicating a tuffaceous origin for the coal samples. Examining the elements’ mode of occurrence suggests their preferential association with mineral matter. Strong positive correlations among elements like Al, K, Na, Ti, Ba, Be, Ni, Cr, Co, Ga, Sc, V, As, Pb, Cu, Zn, and Zr, along with Eu and Sc of the REEs, suggest association with ash yield, consistent with kaolinite and accessory minerals. Comparative analysis of inorganic geochemical composition of coal worldwide reveals notable depletion of major, trace elements, and REEs in samples from all three mines, suggesting limited economic interest. Furthermore, coal samples containing trace elements pose minimal environmental impact.en
dc.identifier.citationJunussov Medet, Tarikhov Farkhad, Abildakhanov Abaidildin, Zhanaidar Dauren, Mekenbek Gulnur, Assambayeva Aizada. (2024). Mineralogical and elemental analysis of Kazakh coals from three mines: Preliminary insights from mode of occurrence to environmental impacts. Open Geosciences. https://doi.org/10.1515/geo-2022-0721en
dc.identifier.doi10.1515/geo-2022-0721
dc.identifier.urihttps://doi.org/10.1515/geo-2022-0721
dc.identifier.urihttps://nur.nu.edu.kz/handle/123456789/10305
dc.language.isoen
dc.publisherWalter de Gruyter GmbH
dc.source(2024)en
dc.subjectKazakhen
dc.subjectMining engineeringen
dc.subjectGeologyen
dc.subjectCoal miningen
dc.subjectMode (computer interface)en
dc.subjectGeochemistryen
dc.subjectEnvironmental scienceen
dc.subjectMineralogyen
dc.subjectArchaeologyen
dc.subjectEarth scienceen
dc.subjectCoalen
dc.subjectGeographyen
dc.subjectComputer scienceen
dc.subjectPhilosophyen
dc.subjectLinguisticsen
dc.subjectOperating system; type of access: open accessen
dc.titleMineralogical and elemental analysis of Kazakh coals from three mines: Preliminary insights from mode of occurrence to environmental impactsen
dc.typearticleen

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