首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Molecular and detailed isotopic structures of petroleum: Kinetic Monte Carlo analysis of alkane cracking
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Molecular and detailed isotopic structures of petroleum: Kinetic Monte Carlo analysis of alkane cracking

机译:石油的分子与详细同位素结构:烷烃裂纹的动力学蒙特卡罗分析

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The compositional and bulk isotopic signatures of hydrocarbon compounds are routinely characterized to constrain the origin of oils and natural gases in sedimentary basins. Recent developments in clumped isotope geochemistry have given rise to a suite of measurements that provide new information on the thermal history of low molecular weight hydrocarbon gases. However, to date no study has linked these compositional, bulk and clumped isotope constraints to any mechanistic understanding of how these signatures develop and evolve. In this study, we developed a kinetic Monte Carlo method to predict consistent and simultaneous molecular distributions, bulk isotopic content, and detailed (multiply substituted and site-specific) isotopic structures of hydrocarbons from a cracking model. The detailed isotopic structure of the source (initially modeled as long alkanes), the intermediates, and the product molecules is followed as a function of the level of conversion due to cracking reactions. The bulk C-13 content of gaseous alkane products generated via the model is shown to follow the linear natural gas plot at low conversion, but to deviate at high conversions. As examples of the information generated, the populations of center vs. terminal C-13-substituted propane are reported as a function of the starting alkane chain length and conversion and the population of doubly-C-13-substituted ethane is described as a function of conversion and for different C-13 substitution patterns in the source. The results are compared to experiment where possible and highlight the possibility of constraining hydrocarbon source isotopic structure and the nature of the generation processes leading to the formation of natural hydrocarbon deposits. (C) 2018 Elsevier Ltd. All rights reserved.
机译:碳氢化合物化合物的组成和散装同位素特征是常规的,以限制沉积盆地中的油和天然气的起源。 Clumped IsoTope地球化学的最新发展已经引起了一套测量,提供有关低分子量烃类气体的热历史的新信息。然而,迄今为止,没有研究将这些组成,散装和团聚同位素的同位素联系起来的任何机械理解,对这些签名如何发展和发展的任何机械理解。在这项研究中,我们开发了一种动力学蒙特卡罗方法,以预测来自开裂模型的一致和同时分子分布,散装同位素含量和详细(多重取代的和位点特异性)同位素结构。源的详细同位素结构(最初建模为长烷烃),中间体和产物分子作为裂化反应引起的转化水平的函数。通过模型产生的气态烷烃产品的体积C-13含量显示在低转化率下的线性天然气曲线,但偏离高转化率。作为产生的信息的实例,作为起始烷烃链长度的函数报告了中心与末端C-13取代丙烷的群体作为起始烷基链长度和转化率和双C-13-取代乙烷的群体被描述为一个功能转换和不同的C-13替换模式在源中。将结果与实验进行比较,尽可能强调约束烃源同位素结构的可能性以及导致形成天然烃沉积物的形成过程的性质。 (c)2018年elestvier有限公司保留所有权利。

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