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Shen Ping, Xu Yongchang. Study on Carbon and Hydrogen Isotopes Composition of Crude Oils[J]. Acta Sedimentologica Sinica, 1998, 16(4): 124-127.
Citation: Shen Ping, Xu Yongchang. Study on Carbon and Hydrogen Isotopes Composition of Crude Oils[J]. Acta Sedimentologica Sinica, 1998, 16(4): 124-127.

Study on Carbon and Hydrogen Isotopes Composition of Crude Oils

  • Received Date: 1998-03-04
  • Publish Date: 1998-08-10
  • In this paper 3 85 crude oil samples from 18 oil-bearing areas of China have been analysed fo r carbon and hydrogen isotopic compositions and part of their saturated and aromatic hydrocarbons have been analy sed fo r carbon isotopic compositions.Based on the analy tical data, the geochemical characteris tics of carbon and hydro- gen isotopes have been s tudied for tw o different types of oils, i.e., normal oil and light oil (condensate)and the hydrocarbon generating organic sources and depositional environments have been discussed combined wi th local geological background.The author propose that the δ13C values of light oil ( condensate)( δ13C-32.5 ‰~ - 24.3‰)are higher than that of normal oil ( δ13C-34.4 ‰~ -24.6‰).The variation of carbon isotopic composi tio ns of aromatic hydrocarbons of crude oils w as obviously affected by the inheritance effect of o rganic Continued on page 144 sources, consequently the δ13C values of aromat ic hy drocarbons could be used to identify crude oils generated from different organic sources. Lig ht oils (co ndensates) related t o marine facies have δD values higher t han - 15 0 ‰, w hereas that related to no nmarine facies have δD values(-21 0 ‰~-1 05 ‰) which basicly cover the δD dist ribution range of marine lig ht oils (condensates).Wit h t he depositional environments changes from fresh w ater to slig htly salt w ater to brackish w ater to marine salt water, δD values of light oils (condensates) become obviously heavier, indicating that δD values mainly related to the depositional environment.
  • [1] 1 C raig H.The geochemist ry of The stable carbon isotopes.GeochiCosmochim A ct a, 1953, (3): 53

    2 D egens E T.Biogeochemist y of stable carbon isotopes.In: Eglington G, M urphey M TJ, eds.O rganic geochemitry.Springer, Berlin-Hei- delberg-N ew york, 1969.5~10

    3 Galimou E M.Larbon isotopes in oil-gas geology.Nedra, M oscow precamb Res, 1973, (5): 221

    4 Stahl W.Carbon isotope in pet roleum geochemist ry.In: Jage E, Hun- zi ker JC, eds.Lecture in isot ope Geology. S ptinger- Verlag, Berlin- Heidelberg-N ew york, 1980.22~25

    5 陈锦石, 陈文石.碳同位素地质学概论.北京: 地质出版社, 1983.2 ~ 5

    6 徐永昌, 沈平, 陈践 发等.凝析油的地球化学特征.中国 科学( B 辑), 1988, ( 6): 634~650

    7 沈平.轻烃中碳 、氢同位素组成特征.中国科学( B 辑), 1993( 11):1216~1226
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  • Received:  1998-03-04
  • Published:  1998-08-10

Study on Carbon and Hydrogen Isotopes Composition of Crude Oils

Abstract: In this paper 3 85 crude oil samples from 18 oil-bearing areas of China have been analysed fo r carbon and hydrogen isotopic compositions and part of their saturated and aromatic hydrocarbons have been analy sed fo r carbon isotopic compositions.Based on the analy tical data, the geochemical characteris tics of carbon and hydro- gen isotopes have been s tudied for tw o different types of oils, i.e., normal oil and light oil (condensate)and the hydrocarbon generating organic sources and depositional environments have been discussed combined wi th local geological background.The author propose that the δ13C values of light oil ( condensate)( δ13C-32.5 ‰~ - 24.3‰)are higher than that of normal oil ( δ13C-34.4 ‰~ -24.6‰).The variation of carbon isotopic composi tio ns of aromatic hydrocarbons of crude oils w as obviously affected by the inheritance effect of o rganic Continued on page 144 sources, consequently the δ13C values of aromat ic hy drocarbons could be used to identify crude oils generated from different organic sources. Lig ht oils (co ndensates) related t o marine facies have δD values higher t han - 15 0 ‰, w hereas that related to no nmarine facies have δD values(-21 0 ‰~-1 05 ‰) which basicly cover the δD dist ribution range of marine lig ht oils (condensates).Wit h t he depositional environments changes from fresh w ater to slig htly salt w ater to brackish w ater to marine salt water, δD values of light oils (condensates) become obviously heavier, indicating that δD values mainly related to the depositional environment.

Shen Ping, Xu Yongchang. Study on Carbon and Hydrogen Isotopes Composition of Crude Oils[J]. Acta Sedimentologica Sinica, 1998, 16(4): 124-127.
Citation: Shen Ping, Xu Yongchang. Study on Carbon and Hydrogen Isotopes Composition of Crude Oils[J]. Acta Sedimentologica Sinica, 1998, 16(4): 124-127.
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