Gas generation of shale organic matter with different contents of residual oil based on a pyrolysis experiment

被引:45
|
作者
Gai, Haifeng [1 ,2 ]
Xiao, Xianming [1 ]
Cheng, Peng [1 ]
Tian, Hui [1 ]
Fu, Jiamo [1 ]
机构
[1] Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, Guangzhou 510640, Guangdong, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
关键词
Shale organic matter; Residual oil; Kerogen; Gas generation; Oil-kerogen interaction; Pyrolysis experiment; FORT-WORTH BASIN; CONFINED PYROLYSIS; ARTIFICIAL MATURATION; BARNETT SHALE; ISOTOPIC REVERSALS; THERMAL-CRACKING; REACTING MEDIUM; SOURCE ROCKS; CARBON; PETROLEUM;
D O I
10.1016/j.orggeochem.2014.11.001
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The generation of gas in organic rich shales with different oil expulsion efficiencies is receiving more attention because of increased global shale gas exploration and development. In this study, a low maturity shale was used to prepare a suite of shale organic matter samples with different contents of residual oil (representative of different oil expulsion efficiencies). These samples were pyrolyzed to investigate the influence of residual oil contents on gas generation and gas chemical and carbon isotopic compositions. The results indicate that with increasing residual oil contents, the total hydrocarbon gas yield (C1-5), heavy hydrocarbon gas yield (C2-5) and gas wetness (C2-5/C1-5) increase, the methane carbon isotopic value (delta C-13(1)%) becomes lighter, and the R-o (vitrinite reflectance) range of the gas window (defined by the main stage of gas generation in the present study) decreases. Through a comparison between the measured data and calculated theoretical values of the hydrocarbon gas yield and methane carbon isotopic values, it is believed that there are interactions between the kerogen and residual oil during gas generation. Although these interactions did not substantially change their hydrocarbon gas potential, there was an influence on the gas generation evolution of the shale organic matter, resulting in a maturity hysteresis of the primary cracking of residual oil to form C2-5 hydrocarbons and a promotion of secondary cracking of the C2-5 hydrocarbons to form methane. These interactions also inhibited the early cracking of kerogen, resulting in more methane generation in the late pyrolysis stage. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:69 / 78
页数:10
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