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

机译:基于热解实验的不同残油含量的页岩有机物产气

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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.
机译:随着全球页岩气勘探和开发的增加,具有不同驱油效率的富含有机质的页岩气的产生越来越受到关注。在这项研究中,低成熟度的页岩被用于制备一套具有不同残留油含量(代表不同排油效率)的页岩有机质样品。对这些样品进行热解,以研究残余油含量对气体产生,气体化学和碳同位素组成的影响。结果表明,随着渣油含量的增加,总烃气收率(C1-5),重烃气收率(C2-5)和气体湿度(C2-5 / C1-5)增大,甲烷碳同位素值( δC-13(1)%变轻,气窗的Ro(镜质体反射率)范围(由本研究中的主要气体生成阶段确定)范围减小。通过将烃气收率和甲烷碳同位素值的测量数据与理论值进行比较,可以认为在产气过程中干酪根和残余油之间存在相互作用。尽管这些相互作用基本上没有改变其烃类气体的潜能,但对页岩有机质的气体生成演化有影响,导致残余油一次裂解形成C2-5烃的成熟滞后,并促进了次生。 C2-5烃裂解生成甲烷。这些相互作用也抑制了干酪根的早期裂解,从而在热解后期产生了更多的甲烷。 (C)2014 Elsevier Ltd.保留所有权利。

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