Molecular and Isotopic Characteristics of Mature Condensates from the East China Sea Shelf Basin Using GC×GC-TOFMS and GC-IRMS

Chao Shan , Jiaren Ye , Alan Scarlett , Kliti Grice

Journal of Earth Science ›› 2019, Vol. 30 ›› Issue (2) : 376 -386.

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Journal of Earth Science ›› 2019, Vol. 30 ›› Issue (2) : 376 -386. DOI: 10.1007/s12583-018-1001-3
Petroleum, Natural Gas Geology

Molecular and Isotopic Characteristics of Mature Condensates from the East China Sea Shelf Basin Using GC×GC-TOFMS and GC-IRMS

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Abstract

In this study, biomarkers, together with stable carbon (δ13C) and hydrogen (δD) isotopic compositions of n-alkanes have been examined in a suite of condensates collected from the East China Sea Shelf Basin (ECSSB) in order to delineate their source organic matter input, depositional conditions and evaluate their thermal maturity. Previously, GC-MS analyses have shown that all the condensates are formed in oxidizing environment with terrestrial plants as their main source input. No significant differences were apparent for biomarker parameters, likely due to the low biomarker content and high maturity of these condensates. Conventional GC-MS analysis however, may provides limited information on the sources and thermal maturity of complex mixtures due to insufficient component resolution. In the current study, we used comprehensive two-dimensional gas chromatography with time-of-flight mass spectrometry (GC×GC-TOFMS) to increase the chromatographic resolution. Compounds such as alkyl cyclohexanes, alkyl cyclopentanes and diamondoids, which can be difficult to identify using conventional GC-MS analysis, were successfully identified using GC×GC-TOFMS. From our analyses we propose two possibly unreported indicators, including one maturity indicator (C5 -cyclohexane/5 +-cyclohexane) and one oxidation-reduction environment indicator (alkyl-cyclohexane/alkyl-cyclopentane). Multiple petroleum charging events were proposed as an explanation for the maturity indicators indexes discrepancy between methyl-phenanthrene index (MPI) and methyl-adamantane index (MDI). In addition, the stable isotopic results show that condensates from the Paleogene have significantly higher positive δ13C values of individual n-alkanes than the Neogene samples. Based on δD values, the samples can be divided into two groups, the differences between which are likely to be attributed to different biosynthetic precursors. Variation within each group can likely be attributed to vaporization.

Keywords

condensate / biomarker characteristic / source information / GC×GC-TOFMS / GC-IRMS

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Chao Shan, Jiaren Ye, Alan Scarlett, Kliti Grice. Molecular and Isotopic Characteristics of Mature Condensates from the East China Sea Shelf Basin Using GC×GC-TOFMS and GC-IRMS. Journal of Earth Science, 2019, 30(2): 376-386 DOI:10.1007/s12583-018-1001-3

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References

[1]

Aguiar A, Aguiar H G M, Azevedo D A, . Identification of Methylhopane and Methylmoretane Series in Ceará Basin Oils, Brazil, Using Comprehensive Two-Dimensional Gas Chromatography Coupled to Time-of-Flight Mass Spectrometry. Energy & Fuels, 2011, 25(3): 1060-1065.

[2]

Aguiar A, Silva A I, Azevedo D A, . Application of Comprehensive Two-Dimensional Gas Chromatography Coupled to Time-of-Flight Mass Spectrometry to Biomarker Characterization in Brazilian Oils. Fuel, 2010, 89(10): 2760-2768.

[3]

Bray E E, Evans E D. Distribution of N-Paraffins as a Clue to Recognition of Source Beds. Geochimica et Cosmochimica Acta, 1961, 22(1): 2-15.

[4]

Chen J H, Fu J M, Sheng G Y, . Diamondoid Hydrocarbon Ratios: Novel Maturity Indices for Highly Mature Crude Oils. Organic Geochemistry, 1996, 25(3/4): 179-190.

[5]

Chikaraishi Y, Naraoka H. Δ13C and ΔD Relationships among Three n-Alkyl Compound Classes (n-Alkanoic Acid, n-Alkane and n-Alkanol) of Terrestrial Higher Plants. Organic Geochemistry, 2007, 38(2): 198-215.

[6]

Cukur D, Horozal S, Lee G H, . Timing of Trap Formation and Petroleum Generation in the Northern East China Sea Shelf Basin. Marine and Petroleum Geology, 2012, 36(1): 154-163.

[7]

Dahl J E, Moldowan J M, Peters K E, . Diamondoid Hydrocarbons as Indicators of Natural Oil Cracking. Nature, 1999, 399(6731): 54-57.

[8]

Dai L M, Li S Z, Lou D, . Numerical Modeling of Late Miocene Tectonic Inversion in the Xihu Sag, East China Sea Shelf Basin, China. Journal of Asian Earth Sciences, 2014, 86: 25-37.

[9]

Dawson D, Grice K, Alexander R. Effect on Maturation on the Indigenous ΔD Signatures of Individual Hydrocarbons in Sediments and Crude Oils from the Perth Basin (Western Australia). Organic Geochemistry, 2005, 36(1): 95-104.

[10]

Dawson D, Grice K, Alexander R, . The Effect of Source and Maturity on the Stable Isotopic Compositions of Individual Hydrocarbons in Sediments and Crude Oils from the Vulcan Sub-Basin, Timor Sea, Northern Australia. Organic Geochemistry, 2007, 38(7): 1015-1038.

[11]

de Rosa M, Gambacorta A, Minale L, . The Formation of Ω-Cyclohexyl-Fatty Acids from Shikimate in an Acidophilic Thermophilic Bacillus. A New Biosynthetic Pathway. Biochemical Journal, 1972, 128(4): 751-754.

[12]

Didyk B M, Simoneit B R T, Brassell S C, . Organic Geochemical Indicators of Paleoenvironmental Conditions of Sedimentation. Nature, 1978, 272(5650): 216-222.

[13]

Fowler M G, Abolins P, Douglas A G. Monocyclic Alkanes in Ordovician Organic Matter. Organic Geochemistry, 1986, 10(4–6): 815-823.

[14]

Freeman K H, Hayes J M, Trendel J M, . Evidence from Carbon Isotope Measurements for Diverse Origins of Sedimentary Hydrocarbons. Nature, 1990, 343(6255): 254-256.

[15]

Grice K, Mesmay R D, Glucina A, . An Improved and Rapid 5A Molecular Sieve Method for Gas Chromatography Isotope Ratio Mass Spectrometry of n-Alkanes (C8−C30 +). Organic Geochemistry, 2008, 39(3): 284-288.

[16]

Hayes J M, Freeman K H, Popp B N, . Compound-Specific Isotopic Analysis: A Novel Tool for Reconstruction of Ancient Biogeochemical Processes. Organic Geochemistry, 1990, 16(4–6): 1115-1128.

[17]

Hayes J M, Takigiku R, Ocampo R, . Isotopic Composition and Probable Origins of Organic Molecules in the Eocene Messel Shale. Nature, 1987, 329(6134): 48-51.

[18]

Inaba T, Suzuki N. Gel Permeation Chromatography for Fractionation and Isotope Ratio Analysis of Steranes and Triterpanes in Oils. Organic Geochemistry, 2003, 34(4): 635-641.

[19]

Johns R B, Belsky T, McCarthy E D, . The Organic Geochemistry of Ancient Sediments II. Geochimica et Cosmochimica Acta, 1966, 30(12): 1191-1222.

[20]

Kikuchi T, Suzuki N, Saito H. Change in Hydrogen Isotope Composition of N-Alkanes, Pristane, Phytane, and Aromatic Hydrocarbons in Miocene Siliceous Mudstones with Increasing Maturity. Organic Geochemistry, 2010, 41(9): 940-946.

[21]

Li C F, Zhou Z, Ge H, . Rifting Process of the Xihu Depression, East China Sea Basin. Tectonophysics, 2009, 472(1–4): 135-147.

[22]

Li M W, Riediger C L, Fowler M G, . Unusual Polycyclic Aromatic Hydrocarbons in the Lower Cretaceous Ostracode Zone Sedimentary and Related Oils of the Western Canada Sedimentary Basin. Organic Geochemistry, 1997, 27(7/8): 439-448.

[23]

Li S F, Hu S Z, Cao J, . Diamondoid Characterization in Condensate by Comprehensive Two-Dimensional Gas Chromatography with Time-of-Flight Mass Spectrometry: The Junggar Basin of Northwest China. International Journal of Molecular Sciences, 2012, 13(9): 11399-11410.

[24]

Li Y, Xiong Y, Chen Y, . The Effect of Evaporation on the Concentration and Distribution of Diamondoids in Oils. Organic Geochemistry, 2014, 69: 88-97.

[25]

Matthews D E, Hayes J M. Isotope-Ratio-Monitoring Gas Chromatography Mass Spectrometry. Analytical Chemistry, 1978, 50(11): 1465-1473.

[26]

Moldowan J M, Seifer W K, Gallegos E J. Relationship between Petroleum Composition and Depositional Environment of Petroleum Source Rocks. American Association of Petroleum Geologists Bulletin, 1985, 69: 1255-1268.

[27]

Oshima M, Ariga T. Cyclohexy1 Fatty Acids in Acidophilic Thermophilic Bacteria. Journal of Biology Chemistry, 1975, 250: 6963-6968.

[28]

Pedentchouk N, Freeman K H, Harris N B. Different Response of δD Values of n-Alkanes, Isoprenoids, and Kerogen during Thermal Maturation. Geochimica et Cosmochimica Acta, 2006, 70(8): 2063-2072.

[29]

Powell T G, McKirdy D M. Relationship between Ratio of Pristane to Phytane, Crude Oil Composition and Geological Environment in Australia. Nature, 1973, 243(124): 37-39.

[30]

Radke J, Bechtel A, Gaupp R, . Correlation between Hydrogen Isotope Ratios of Lipid Biomarkers and Sediment Maturity. Geochimica et Cosmochimica Acta, 2005, 69(23): 5517-5530.

[31]

Rubinstein I, Strausz O P. Geochemistry of the Thiourea Adduct Fraction from an Alberta Petroleum. Geochimica et Cosmochimica Acta, 1979, 43(8): 1387-1392.

[32]

Schaeffer P, Poinsot J, Hauke V, . Novel Optically Active Hydrocarbons in Sediments: Evidence for an Extensive Biological Cyclization of Higher Regular Polyphenols. Angewandte Chemie, 1994, 33(11): 1166-1169.

[33]

Schimmelmann A, Sessions A, Boreham C J, . D/H Ratios in Terrestrially Sourced Petroleum Systems. Organic Geochemistry, 2004, 35(10): 1169-1195.

[34]

Seifert W K, Moldowan J M. Use of Biological Markers in Petroleum Exploration. Methods in Geochemistry and Geophysics, 1986, 24: 261-290.

[35]

Spiro B. Effects of the Mineral Matrix on the Distribution of Geochemical Markers in Thermally Affected Sedimentary Sequences. Organic Geochemistry, 1984, 6: 543-559.

[36]

Tang Y C, Huang Y S, Ellis G S, . A Kinetic Model for Thermally Induced Hydrogen and Carbon Isotope Fractionation of Individual n-Alkanes in Crude Oil. Geochimica et Cosmochimica Acta, 2005, 69(18): 4505-4520.

[37]

Triwahyono, S., Abdul, J. A., Shamsuddin, M., et al., 2005. Isomerization of Cyclohexane to Methylcyclopentane over Pt/sulfate-ZrO2 Catalyst. 2nd International Conference on Chemical and Bioprocess Engineering, Sabah

[38]

Ventura G T, Raghuraman B, Nelson R K, . Compound Class Oil Fingerprinting Techniques Using Comprehensive Two-Dimensional Gas Chromatography (GC×GC). Organic Geochemistry, 2010, 41(9): 1026-1035.

[39]

Ventura G T, Simoneit B R T, Nelson R K, . The Composition, Origin and Fate of Complex Mixtures in the Maltene Fractions of Hydrothermal Petroleum Assessed by Comprehensive Two-Dimensional Gas Chromatography. Organic Geochemistry, 2012, 45: 48-65.

[40]

Wang T G, Zhong N N, Huo D J, . Several Genetic Mechanisms of Immature Crude Oils in China. Acta Sedimentologica Sinica, 1997, 2: 75-83. (in Chinese with English Abstract)

[41]

Wang Y, Huang Y. Hydrogen Isotopic Fractionation of Petroleum Hydrocarbons during Vaporization: Implications for Assessing Artificial and Natural Remediation of Petroleum Contamination. Applied Geochemistry, 2003, 18(10): 1641-1651.

[42]

Wei Z B, Moldowan J M, Jarvie D M, . The Fate of Diamondoids in Coals and Sedimentary Rocks. Geology, 2006, 34(12): 1013-1023.

[43]

Wei Z B, Moldowan J M, Zhang S C, . Diamondoid Hydrocarbons as a Molecular Proxy for Thermal Maturity and Oil Cracking: Geochemical Models from Hydrous Pyrolysis. Organic Geochemistry, 2007, 38(2): 227-249.

[44]

Williams J A, Dolcater D L, Torkelson B E, . Anomalous Concentrations of Specific Alkylaromatic and Alkylcycloparaff in Components in West Texas and Michigan Crude Oils. Organic Geochemistry, 1988, 13(1–3): 47-60.

[45]

Yang S C, Hu S B, Cai D S, . Present-Day Heat Flow, Thermal History and Tectonic Subsidence of the East China Sea Basin. Marine and Petroleum Geology, 2004, 21(9): 1095-1105.

[46]

Ye J R, Chen H H, Chen J Y, . Fluid History Analysis in the Xihu Depression, East China Sea. Natural Gas Industry, 2006, 26(9): 40-43. (in Chinese with English Abstract)

[47]

Zhu C S, Zhao H, Wang P R, . The Distribution and Carbon Isotopic Composition of Unusual Polycyclic Alkanes in the Cretaceous Lengshuiwu Formation, China. Organic Geochemistry, 2003, 34(7): 1027-1035.

[48]

Zhu Y, Li Y, Zhou J, . Geochemical Characteristics of Tertiary Coal-Bearing Source Rocks in Xihu Depression, East China Sea Basin. Marine and Petroleum Geology, 2012, 35(1): 154-165.

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