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Ding Anna, Hui Rongyao, Zhang Zhongning, Duan Yi. Stable Carbon Isotope Compositions of Liquid Hydrocarbon Molecules and their Application[J]. Acta Sedimentologica Sinica, 1996, 14(1): 135-142.
Citation: Ding Anna, Hui Rongyao, Zhang Zhongning, Duan Yi. Stable Carbon Isotope Compositions of Liquid Hydrocarbon Molecules and their Application[J]. Acta Sedimentologica Sinica, 1996, 14(1): 135-142.

Stable Carbon Isotope Compositions of Liquid Hydrocarbon Molecules and their Application

  • Received Date: 1994-12-04
  • Publish Date: 1996-03-10
  • This paper reports carbon isotopic compositions of individual n-alkanes and isoprenoids from crude oil and source rock samples in the Junggar Basin. Between nC11 and nC34 , the most part of isotopic compositions of n-alkanes originating from the Jurassic limnetic factes is-27.0‰, to-32.4‰,,heavier than that of the crude oil from the marine factes strata, characterized by 13C-rich isotope.The n-alkane δ13C values of the crude oil from the type Ⅱ A source rock are lighter than that of the type Ⅱ B oil, it suggests that n-alkane be richer in 12C relatively.If crude oils are derived from the same group of organism or,at least,from organism using the same carbon source, the δ13C values of these n-alkanes and isoprenoids have a similar distributional range and total variational trend. Therefore, these data can be used in the source rock/oil correlation.The isotopic compositions of individual n-alkanes of the oil from the Cainan oil field become similar to that from the lower Jurassic Sangonghe source rock, they show a variation from-26.0‰,to-32.0‰,in the nC11 to nC32 range, among the same carbon numbers, the δ13C differences is less than 2‰,especially the δ13C value of n-alkanes in the Cainan oil matches that in the saturated hydrocarbon fractions from the lower Jurassic Sangonghe source rock.In the Pencan-2 well, the δ13C values of crude oil n-alkanes coincide with that of the Badaowan source.The Du-71 well is located on the southern margin of the Junggar Basin, its productive strata are shallower.The δ13C values of C11 -C23 n-alkanes vary from heavier to lighter with increasing of the carbon number, ranging from - 25. 4‰, to - 33.0‰, These values have a similar trend to the Toutunhe source rock. Through the study on microbiology, it has been proved that there is a great amount of Methanococcus in the Toutunhe hydrocarbon source rock.Therefore, the origin of the Dushanzi oil is possibly related to archaeobacteria.
  • [1] 1.张文正,裴戈,关德师,液态正构烷烃系列、姥绞烷、植烷碳同位素初步研究,石油勘探与开发,1992. 19(5):32 -41。

    2.Collister, J. W. et al.,An isotopic biogeochemical study of the Green River oil shale. Organic Geochemistry. 1992, 19(1一3):265一276.

    3.Bjorvy,M. et al.,Variation in stable carbon isotope ratios of individual hydrocarbons as a function of ar-tificial maturity. Organic Geochemistry.1992,19(1一3):89一105.
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  • Received:  1994-12-04
  • Published:  1996-03-10

Stable Carbon Isotope Compositions of Liquid Hydrocarbon Molecules and their Application

Abstract: This paper reports carbon isotopic compositions of individual n-alkanes and isoprenoids from crude oil and source rock samples in the Junggar Basin. Between nC11 and nC34 , the most part of isotopic compositions of n-alkanes originating from the Jurassic limnetic factes is-27.0‰, to-32.4‰,,heavier than that of the crude oil from the marine factes strata, characterized by 13C-rich isotope.The n-alkane δ13C values of the crude oil from the type Ⅱ A source rock are lighter than that of the type Ⅱ B oil, it suggests that n-alkane be richer in 12C relatively.If crude oils are derived from the same group of organism or,at least,from organism using the same carbon source, the δ13C values of these n-alkanes and isoprenoids have a similar distributional range and total variational trend. Therefore, these data can be used in the source rock/oil correlation.The isotopic compositions of individual n-alkanes of the oil from the Cainan oil field become similar to that from the lower Jurassic Sangonghe source rock, they show a variation from-26.0‰,to-32.0‰,in the nC11 to nC32 range, among the same carbon numbers, the δ13C differences is less than 2‰,especially the δ13C value of n-alkanes in the Cainan oil matches that in the saturated hydrocarbon fractions from the lower Jurassic Sangonghe source rock.In the Pencan-2 well, the δ13C values of crude oil n-alkanes coincide with that of the Badaowan source.The Du-71 well is located on the southern margin of the Junggar Basin, its productive strata are shallower.The δ13C values of C11 -C23 n-alkanes vary from heavier to lighter with increasing of the carbon number, ranging from - 25. 4‰, to - 33.0‰, These values have a similar trend to the Toutunhe source rock. Through the study on microbiology, it has been proved that there is a great amount of Methanococcus in the Toutunhe hydrocarbon source rock.Therefore, the origin of the Dushanzi oil is possibly related to archaeobacteria.

Ding Anna, Hui Rongyao, Zhang Zhongning, Duan Yi. Stable Carbon Isotope Compositions of Liquid Hydrocarbon Molecules and their Application[J]. Acta Sedimentologica Sinica, 1996, 14(1): 135-142.
Citation: Ding Anna, Hui Rongyao, Zhang Zhongning, Duan Yi. Stable Carbon Isotope Compositions of Liquid Hydrocarbon Molecules and their Application[J]. Acta Sedimentologica Sinica, 1996, 14(1): 135-142.
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