Advanced Search

LI Chun yuan, WANG Xian bin, XIA Xin yu. The Possibility and Explanation of Complete Reverse Isotopi c Distribution of Light Hydrocarbons in Natural Gas[J]. Acta Sedimentologica Sinica, 1999, 17(2): 306-311.
Citation: LI Chun yuan, WANG Xian bin, XIA Xin yu. The Possibility and Explanation of Complete Reverse Isotopi c Distribution of Light Hydrocarbons in Natural Gas[J]. Acta Sedimentologica Sinica, 1999, 17(2): 306-311.

The Possibility and Explanation of Complete Reverse Isotopi c Distribution of Light Hydrocarbons in Natural Gas

  • Received Date: 1998-11-12
  • Publish Date: 1999-06-10
  • Carbon isotope distribution among the C1 to C4 hydrocarbon is one of the most important criteria to identify the genesis of natural gas.Generally,bio genic natural gases possess a “normal distribution ”in carbon isotopes of C 1 to C4 hydrocarbons and abiogenic natual gases a “reversal distribution”in carbon isotopes of C1 to C4 hydrocarbons.Some scholars consider that “isot opic reversals”can result from the mixture of two kinds of biogenic natural gas with “normal distribution” in carbon isotope.However,prevenient numerical sim ulation did not confim the viewpoint.By means of numerical simulation,the possib ility of “isotopic reversals” in C1 to C4 hydrocarbons resulted from the mixture of two kinds of biogenic natural gas was discussed in this paper. Computation in this article shows that a complete reverse carbon isotopic distri bution among C1 to C4 hydrocarbons (i.e. δ13C methane >δ13 C propane >δ13C n-butane) can be produced by the mixture of two kinds of biogenic gas with a normal carbon isotopic distribution (i.e. δ13C m ethane <δ13C ethane <δ13 propane <δ13C n-butane). While a normal carbon isotopic distribution in natural gas can also be produced by two e ndmembers with reverse distributions. As for the first case, the two endmembers should be of different source, different formation, or of different evolutional stage. It is unreasonable to explain the isotopic reverse distribution of the gas sampl es from several wells of the Changde pool, Songliao Basin by the mixture model, because the isotopically higher endmember needed to form this real gas is not fo und in Songliao Basin. So a better explanation to the isotopic reversal in this gas pool is to consider it to be abiogenic.
  • [1] Chung H M, Gormly J R, Squires R M, Origin of gaseous hydroc arbons in subsurface environments; theoretical considerations of carbon isotope distribution[J] . Chemical Geology, 1988, 71∶ 97~103
    [2] McCarty H B, Felbeck G T, High temperature simulation of petroleum for mation-Ⅳ. Stable carbon isotope studies of gaseous hydrocarbons[J] . Organic G eochemistry, 1986, 9∶ 183-192
    [3] James A T. Correlation of natural gas by use of carbon isotopic distr ibution between hydrocarbon components[J] . American Association of Petroleum G eologists Bulletin, 1983, 67∶ 1176~1991
    [4] Galimov E M. Sources and mechanisms of formation of gaseous hydrocarb ons in sedimentary rocks[J] . Chemical Geology. 1988, 71∶77~95
    [5] Clayton C. Carbon isotope fractionation during natural gas generation from kerogen[J] . Marine and Petroleum Geology. 1991, 8∶232~240
    [6] Des Marais D J, Donchin J H, Nehring N L et al. Molecular car bon isotopic evi dence for the origin of geothermal hydrocarbons[J] . Nature, 1981, 292∶ 826~8 28
    [7] Chang S, Des Marais D J, Mack R, Prebiotic organic synthesis and the o rigin of life[A] . In: Schopf J W, ed, Earth's earliest biosphere, its origin and evolution[C] . Princeton, N J, Princeton University Press, 1983. 54~92
    [8] Galimov E M, Carbon isotopes in oil-gas geology[R] . U.S. Department of Commerce, National Technical Information Service, N75-27563, 1975, 395
    [9] Konnerup_Madsen J, Kreulen R, Rose-Hansen J. Stable isotope character istics of hydrocarbon gases in the alkaline Ilimaussaq complex, South Greenland [J] . Bulletin de Mineralogie, 1988, 111∶ 567-576
    [10] Yuen G, Blair N, Des Marais D J,Chang S. Carbon isotope compositio n of low molecular weight hydrocarbons and monocarboxylic acids from Murchi son meteorite[J] . Nature,1984, 307∶ 252~254
    [11] Fuex A N. The use of stable carbon isotopes in hydrocarbon explorati on[J] . Journal of Geochemical Exploration, 1977, 7∶ 155~188
    [12] Schoell M. Wasserstoff-and Kohlenstoff Isotope in organischen Substan zen, Erdolen and Erdgasen[J] . Geologisches Jahrbuch, 1984, D 67∶164
    [13] Jenden P D, Kaplan I R. Origin of natural gas in the Sacramento basin, California[J] . American Association of Petroleum Geologists Bulletin, 1 989, 73∶ 431~453
    [14] Des Marais D J, Stallard M L, Nehring N L, Truesdell A H. Carbon iso tope geochemistry of hydrocarbons in the Cerro Prieto geothermal field, Baja Cal ifornia Norte, Mexico[J] . Chemical Geology, 1988, 71∶ 159~167.
    [15] James A T, Burns B J. Microbial alteration of subsurface natura l gas accumulations[J] . American Association of Petroleum Geologists Bulletin, 1984, 68∶ 957~960.
    [16] 郭占谦,王先彬.松辽盆地非生物成因气的探讨[J] .中国科学,1994,3:30 3~309.
    [17] Jenden P D, Hilton D R, Kaplan I R, Craig H. Abiogenic hydroca rbons and mantle helium in oil and gas fields[A] , In: David G H, et al, eds . The Future of Energy Gases[C] . 1994. 31~56.
    [18] 戴金星. 天然气碳氢同位素特征和各类天然气鉴别[J] . 天然气地球科学,19 93,(2)∶1~40.
    [19] 徐永昌. 天然气成因理论及应用[M] . 北京:科学出版社,1994.84~101
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(505) PDF downloads(508) Cited by()

Proportional views
Related
Publishing history
  • Received:  1998-11-12
  • Published:  1999-06-10

The Possibility and Explanation of Complete Reverse Isotopi c Distribution of Light Hydrocarbons in Natural Gas

Abstract: Carbon isotope distribution among the C1 to C4 hydrocarbon is one of the most important criteria to identify the genesis of natural gas.Generally,bio genic natural gases possess a “normal distribution ”in carbon isotopes of C 1 to C4 hydrocarbons and abiogenic natual gases a “reversal distribution”in carbon isotopes of C1 to C4 hydrocarbons.Some scholars consider that “isot opic reversals”can result from the mixture of two kinds of biogenic natural gas with “normal distribution” in carbon isotope.However,prevenient numerical sim ulation did not confim the viewpoint.By means of numerical simulation,the possib ility of “isotopic reversals” in C1 to C4 hydrocarbons resulted from the mixture of two kinds of biogenic natural gas was discussed in this paper. Computation in this article shows that a complete reverse carbon isotopic distri bution among C1 to C4 hydrocarbons (i.e. δ13C methane >δ13 C propane >δ13C n-butane) can be produced by the mixture of two kinds of biogenic gas with a normal carbon isotopic distribution (i.e. δ13C m ethane <δ13C ethane <δ13 propane <δ13C n-butane). While a normal carbon isotopic distribution in natural gas can also be produced by two e ndmembers with reverse distributions. As for the first case, the two endmembers should be of different source, different formation, or of different evolutional stage. It is unreasonable to explain the isotopic reverse distribution of the gas sampl es from several wells of the Changde pool, Songliao Basin by the mixture model, because the isotopically higher endmember needed to form this real gas is not fo und in Songliao Basin. So a better explanation to the isotopic reversal in this gas pool is to consider it to be abiogenic.

LI Chun yuan, WANG Xian bin, XIA Xin yu. The Possibility and Explanation of Complete Reverse Isotopi c Distribution of Light Hydrocarbons in Natural Gas[J]. Acta Sedimentologica Sinica, 1999, 17(2): 306-311.
Citation: LI Chun yuan, WANG Xian bin, XIA Xin yu. The Possibility and Explanation of Complete Reverse Isotopi c Distribution of Light Hydrocarbons in Natural Gas[J]. Acta Sedimentologica Sinica, 1999, 17(2): 306-311.
Reference (19)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return