Origin of Condensate Gas in Bozhong 19-6 Gas Field in Bohai Bay Basin
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CNOOC Research Institute Co., Ltd.,China National Offshore Oil Corporation, Beijing 100028, China

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T122

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    Abstract:

    In order to analyze the genesis and source of Bozhong 19-6 gas condensate reservoir, the genesis and gas-oil relationship of Bozhong 19-6 gas reservoir were analyzed using a series of isotopes, light hydrocarbon parameters, and biomarkers.The results show that Bozhong 19-6 gas field has a low drying coefficient, a heavy carbon isotope, and a maturity distribution of about 1.50 %, representing a hybrid origin and high-mature gas. The content of dicamantane in the condensate from Bozhong 19-6 gas field is high whereas the content of biomarkers is low, showing a characteristic of high-mature oil. This indicates that the cracking degree of normal oil amounts is lower than 20 %. The contribution of natural gas produced from cracking of crude oil is small. The gas in Bozhong 19-6 gas field is mainly formed by kerogen cracking.

    Table 1
    Fig.1 Location of Bozhong 19-6 gas condensate field
    Fig.2 Carbon isotope genetic identification of Bozhong 19-6 gas field
    Fig.3 Light hydrocarbon system triangle chart of Bozhong 19-6 gas field
    Fig.4 Cross plots of w(P2 + N2)/w(T) versus w(P3) /w(T)and w(N2/ w(P3) versus w(P2)/w(T) of piedmont zone of Bozhong 19-6 gas field
    Fig.5 Partial humus type gas maturity identification of Bozhong 19-6 gas field
    Fig.6 δ13C1 versus δ13C2 -δ13C1 carbon isotope of natural gas
    Fig.7 Oil cracking degree versus amantadane content
    Fig.8 Extent of cracking versus methyldiamantane concentration in laboratory oil-cracking experiments
    Fig.9 Geothermal evolution history of Bozhong 19-6 structure
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LI Wei. Origin of Condensate Gas in Bozhong 19-6 Gas Field in Bohai Bay Basin[J].同济大学学报(自然科学版),2021,49(3):458~466

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History
  • Received:November 18,2019
  • Online: April 06,2021
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