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Kinetic modelling of kerogen cracking during oil shale process : influence of organic matter source

机译:油页岩过程干酪根裂解动力学模型:有机物源的影响

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1. First step : kerogen cracking 1.1 Most of the asphaltenes are degraded 1.2 Resins are more stable class 1.3 C_(14+) aromatics start to be cracked at high kerogen conversion 1.4 C_(14+) saturates are almost stable Still high content in -NSOs (asp + resins): production of low °APi and low mobility fluid, → significant secondary cracking reaction 2. Second step : influence of the secondary cracking reaction 2.1 Available compositional kinetic schema.
机译:1.第一步:干酪根裂解1.1大多数沥青质被降解1.2树脂更稳定1.3级C_(14+)芳烃在较高的干酪根转化率下开始裂解1.4 C_(14+)饱和物几乎稳定在- NSO(asp +树脂):产生低°APi和低迁移率的流体,→发生明显的二次裂化反应2.第二步:二次裂化反应的影响2.1可用的组成动力学图式。

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