Chemical Composition and Their Geochemical Feature in Two Special Coal Extracts of Hunyuan Coal and Lupinite-Alkane Fraction
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摘要: 本文利用GC和GC/MS技术对山西浑源藻烛煤和江西东中树皮煤的索氏抽提物的烷烃镏分进行了研究。首次发现浑源藻烛煤中存在显著量的C28二降藿烷,伽马蜡烷和γ-戎萝卜烷,而在乐平树皮煤中却不存在可检测量的甾烷系列。Abstract: The present paper investigated the extracts of mathanol-benzene soxhlet extraction for two extraordinary coals, namely, a Hunyuan algel candle in Shanxi Province and Lupinite in Jiangxi Province. by means of gas chromatography, and GC/MS techniquts. The chemical structures and configulation were identified by Kovats Values of gas chromatograms, mass chromatograms and the interpretation of mass fragmentagrams. The occurrence and distrbution feature of alkanes, isoprenoids, alkyl cycolhexanes, terpanes and steranes have been investigated. The correlalionship between some geochemical parameters and precursor of coal-original as well as sedimentary environment was discussed. Hunyuan algal candle is a sapropelic coal with higher H/C and O/ C atomic ratios(1.13 and 0.18 respectively) and there are many algae and waxes under the microscopic study. The conspicuously present of 17αH, 18αH, 21βH-28, 30-C28 bisnorhopane, gammacerane and γ-carotane have been firstly identi fied in this kind of boghead coal. Some geochemical parameters, such as pristane/phytane = 0.5, ∑ C20/ ∑C20+= 1. 04, C29-xxx-( R+ S)/C27- xxx-( R+ S) = 1. 66, index of gammacerane(gammacerane/ C30-xβhopane) =0.23, the ratio of 22S to 22R for C32-C35 hopane 1 and a few percentage of C15-C22 alkylcyclohexane as well as completely sterane system indicated that the paleoenvironment of Hunyuan algal candle was a reducing environment covered by saline water, the main input precursor is higher plant followed by algae and bacteria. Lupinite from Jinxi is an unique bark coal which is referred as Lupinite as new coal macerals in the petrography. In the alkane fraction of benzene- methanol extract from Lupinite, there are some geochemical characters as follows: a lack of sterane system is a quite special case in the coal extraction. n-C160is main component in the normal alkane, ∑C20-/ ∑ C20+= 3.2, Pr/Ph= 1.3, C12-C20 alkyl cyclohexane account 4%, the distribution of carbon number of alkyl cyclohexane as same as normal alkane, but the main peak is C15, one carbon number less than normal alkane. The ratio of 22S to 22R for C32-C35 hopane 1. The microscopic study indicated that Lupinite consists mainly of suberinite of Lepidodendrales and ferns as the primordial plant debris(account 50-70%) with decken structure due to paralic deposit environment in which both aerobic and anaerobic environment would be alternatively existed, therefore, both aerobic and anaerobic bacteria attacked the plant debris where completely decomposition of celluloses and lignin would be happened and only preserved stable exinite and suberinite as resi dues.
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[1] (1) 工锐良、尚慧芸、傅家谟,盛国英,1990.中国科字院地化所有机地球化学开放实验研究年报1988,科学出版社,100-107页
(2) 史继杨,1986.有机地球化学论文集.科学出版社59-67页
(3) 孙玉麟、顾永达、吴奇虎,1988,燃料化学学报16卷, 136- 142页
(4) 顾永达,王郁.姜德福,1988.然料化学学报14卷,69-83页
(5) 黄第涛,李晋超,周翥虹.顾信章.张大江、1984.陆相有机质演化和成烃机钾 石油工业出版社,50-54页
(6)傅家说 .盛国英,1986,中国主要含油(盆地沉积类型的有机地球化学特征.有机地球化学沦文集.科学出版社1-17页
(7) 曾宪章、王忠然、张振才,陈献忠.,刘淑珍,1986.有机地球化学论文集,科学出版社38-49 页
(8) 菲尔普、PR,1987'.化石燃科生物标志物-应用与谱图,傅家谟.盛国英译1987'.科学出版社 71-77页
(9) Didyk B,M., Simonet B R T,Rrasell S C and Eglinton G .1978. Nature.V.272 p216-222页
(10) Gruntham P J .Pasthuma J., and De Groot K. 1980. In: Advances In the organic Geochemistry1979..A.G., Douglas and J.R . Maxwell eds. P.29-38
(11) Hsleh C.Y .,1933 Bull Geo. Soc China.V.12.p.469-490.
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