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利用红外光谱剖析干酪根三类主要原子团的演化 被引量:3

DISSECTING THE EVOLUTION OF THREE MAIN ATOMIC GROUPS OF KEROGEN BY FTIR
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摘要 作者用红外光谱仪分析了泌阳凹陷生油岩干酪根,研究了干酪根中烷基、含氧官能团和芳环的变化规律。含氧官能团随埋深逐渐减少,到达一定深度后完全消失;烷基具有明显的高峰区,这个高峰与生油高峰是一致的;芳环在生油门限前后比较稳定,生油高峰过后明显增加。 The authors studied 41 samples of kerogen from the Eogene HetaoyuanFormation in Biyang Depression,Henan by ETIR technique.Oxygen-bearingfunctional group decreases with the increase of buried depth,and completelydisappeared at 3500m.Alkyl group increases to a peak value with theincrease of buried depth,and then decreases gradually.The depth of peak-value shows identity with that of oil-generating peak.Aromatic rings showa little change near the threshold depth of oil-generation but increases obvi-ously below the depth of oil-generation peak.
作者 杨志琼 章聆
出处 《石油与天然气地质》 EI CAS CSCD 北大核心 1989年第1期53-58,共6页 Oil & Gas Geology
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同被引文献27

  • 1邹艳荣,帅燕华,孔枫,彭平安.油气生成过程实验研究的思考与展望[J].石油实验地质,2004,26(4):375-382. 被引量:30
  • 2Behar F and Vandenbroucke M. Chemical modelling of kerogens. Organic Geochemistry, 1987, 11:15~24
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  • 7Landiais P and Rochdi A. Reliability of semi-quantitative data extracted from transmission microscopy Fourier transform infrared spectra of coal. Energy & Fuels, 1990, 4(3): 290~295
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  • 9傅家谟, 秦匡宗. 干酪根地球化学. 广州:广东科技出版社,1995[Fu Jiamo, Qing Kuangzong. Kerogen Geochemistry. Guangzhou: Guangdong Science & Technology Press, 1995]
  • 10Ganz H and kalkrenth W. kerogen-type and the evaluation of source rock and oil shale potentials. Fuel, 1987, 66:708~711

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