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Geochemical and isotopic characterization of coalbed gases in active excavation fields at Preloge and Pesje (Velenje Basin) mining areas

机译:Preloge和Pesje(Velenje盆地)矿区活跃挖掘场中煤层气的地球化学和同位素特征

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摘要

Coalbed gases in excavation fields of mining areas in the Velenje coal basin have been subjected to geochemical and isotopic monitoring since the year 2000, with the aim of obtaining better insights into the origin of coalbed gases. Results from active excavation fields in the mining areas Pesje and Preloge in the year 2013 are presented in this study. Composition and isotopic composition of coalbed gases were determined with methods utilizing mass spectrometry. The chemical and isotopic composition of coalbed gases in the Velenje Basin vary and depend on the composition of the source of coalbed gas before excavation, advancement of the working face, depth of the longwall face, pre-min-ing activity and newly mined activity. The basic gas components determined in excavation fields are CO2 and methane. The isotopic composition of deuterium in methane has been determined and used to characterize the origin of methane. The isotopic compositions of carbon and hydrogen in methane in the excavation fields show its biogenic origin, while a high Carbon Dioxide Methane Index indicates the bacterial and endogenic origin of CO2.
机译:自2000年以来,维伦耶(Velenje)煤盆地矿区开挖场中的煤层气一直受到地球化学和同位素监测,目的是更好地了解煤层气的成因。这项研究介绍了2013年Pesje和Preloge矿区活跃挖掘场的结果。用质谱法确定煤层气的组成和同位素组成。 Velenje盆地中煤层气的化学和同位素组成各不相同,并取决于开挖前煤层气源的组成,工作面的推进,长壁工作面的深度,开采前的活动和新开采的活动。在挖掘现场确定的基本气体成分是CO2和甲烷。已确定甲烷中氘的同位素组成,并用于表征甲烷的来源。开挖场中甲烷中碳和氢的同位素组成显示出其成因,而较高的二氧化碳甲烷指数表明了CO2的细菌和内源。

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