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首页> 外文期刊>Journal of the Serbian Chemical Society >Characterisation of lignite lithotypes from the “Kovin” deposit (Serbia) - implications from petrographic, biomarker and isotopic analysis
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Characterisation of lignite lithotypes from the “Kovin” deposit (Serbia) - implications from petrographic, biomarker and isotopic analysis

机译:“ Kovin”矿床(塞尔维亚)中褐煤岩型的表征-岩石学,生物标志物和同位素分析的意义

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摘要

Four lignite lithotypes (matrix coal, xylite-rich coal, mixture of matrix and mineral-rich coal and mixture of matrix and xylite-rich coal), originating from the Kovin deposit, were investigated in detail. The paper was aimed to determine the main maceral, biomarker and isotopic (δ13C) characteristics of investigated lithotypes. Based on these results the sources and depositional environment of organic matter in 4 lithotypes were established. These samples were also used as substrates for investigation of the influence of diagenetic alteration on δ13C signatures of biomarkers, as well as for assessment of the most convenient utilization for each lithotype. The investigated lithotypes differ in accordance with the composition of huminite macerals. Xylite-rich coal notably distinguishes from other lithotypes beacuse of the highest content of conifer resins vs. epicuticular waxes. The mixture of matrix and mineral-rich coal is characterised by the greatest contribution of algae and fungi and the most intense methanotrophic activity at the time of deposition. In all coal lithotypes diagenetic aromatisation influenced isotopic composition of individual biomarkers. Xylite-rich coal has the poorest grindability properties. However, this coal lithotype is the most suitable for fluidized bed gasification, whereas the mixture of matrix and mineral-rich coal has the lowest applicability for this process. The calorific value decreases in order: xylite-rich coal > matrix coal > mixture of matrix and xylite-rich coal > mixture of matrix and mineral-rich coal. The increase of organic carbon content and calorific value is controlled by the increase of contribution of wood vegetation vs. herbaceous peat-forming plants, as well as by stability of water table during peatification. [Project of the Ministry of Education, Science and Technological Development of the Republic of Serbia, Grant no. 176006 and Grant no. 451-03-01039/2015-09/05]
机译:详细研究了源自科文矿床的四种褐煤岩型(基质煤,富黄铁矿煤,基质与富矿物质的混合物以及基质与富黄铁矿的混合物)。本文旨在确定所研究岩石类型的主要组成,生物标志物和同位素(δ13C)特征。根据这些结果,建立了四种岩性有机质的来源和沉积环境。这些样品还用作底物,以研究成岩作用变化对生物标记物δ13C标记的影响,以及评估每种岩型的最方便利用。所研究的岩性根据腐殖质微石的组成而有所不同。富含木蜡矿的煤与针石树脂和表皮蜡相比含量最高,这与其他岩性明显不同。基质和富含矿物质的煤的混合物的特征在于,沉积时藻类和真菌的贡献最大,甲烷营养最强。在所有煤岩型中,成岩作用都影响单个生物标记物的同位素组成。富含木蜡矿的煤的可磨性最差。但是,这种煤岩型最适合流化床气化,而基质和富含矿物质的煤的混合物在该过程中的适用性最低。热值按以下顺序递减:富黄铁矿煤>基质煤>基质与富黄铁矿煤的混合物>基质与富矿物质的煤的混合物。有机碳含量和热值的增加是由木材植被对草本泥炭形成植物的贡献增加以及在泥炭化过程中地下水位的稳定性控制的。 [塞尔维亚共和国教育,科学和技术发展部的项目,批准号: 176006和授权号451-03-01039 / 2015-09 / 05]

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