Organic geochemistry of the Late Permian coals from the Huoshaopu and Jinjia Mines, Liupanshui Coalfield, China. Issue 6 (November 2016)

• Record Type: Journal Article
• Authors: Qin, Shenjun; Gao, Kang; Wang, Jinxi; Li, Yanheng; Lu, Qingfeng
• Is Part Of: Energy exploration & exploitation. Volume 34:Issue 6(2016)
• Page Start: 881
• Page End: 898
• Publication Date: 2016-11
• Subjects: Liupanshui coalfield -- bituminous coal -- hydrocarbon distribution -- molecular parameter; Power resources -- Periodicals; 333.79
• DOI: 10.1177/0144598716665019
• Languages: English
• ISSNs: 0144-5987

Abstract

Four coal samples from the Huoshaopu Mine and six coal samples from the Jinjia Mine, Liupanshui Coalfield, China were collected and analyzed, focusing on their petrological and organic geochemical features. The microscopic results show that the vitrinite random reflectance ( R o ) of all samples is 0.97%, which is classified as high-volatile A bituminous coal. The maceral groups are dominated by vitrinite followed by inertinite. The low ratios (0.07–0.42) of saturated to aromatic hydrocarbons indicate a terrestrial plant input for the coals. Gas chromatography and gas chromatography/mass spectrometry were employed to analyze the composition of organic matter in the samples. The gas chromatography chromatograms of saturates display a monomodal outline of n -alkanes with a predominance of short chains. The odd-even preference values around 1 reflect the thermal maturity of the coals. Based on the different pristine/phytane ratios and dibenzofuran contents, we infer a relatively weak oxic coal-forming environment for Huoshaopu coals and a relatively anoxic environment for Jinjia coals. Among the aromatics, thermodynamically stable compounds, including 2-methylnaphthalene, 2, 6 + 2, 7-dimethylnaphthalenes, 3 and 4-methylbiphenyls, 4, 4′-dimethylbiphenyl, methylphenanthrene, 2 and 3-methyldibenzofurans, were the dominant isomers in the respective homologs. The occurrence of dibenzothiophenes and benzonaphthothiophenes may confirm the paralic depositional environment of Late Permian coals from the Huoshaopu and Jinjia mines.