岩浆动力学分布和模拟为了解富含有机质页岩的石油转化率 (TF) 剖面提供了启示

IF 4.1 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
David A. Wood
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引用次数: 0

摘要

模拟了 250 个一阶阿伦尼乌斯反应,在 25、15 和 5 °C-min-1 三种加热速率下生成 S2 高温图。模拟反应的活化能(E)和预指数(A)与页岩和角砾岩的可变值趋势一致。将模拟的单一反应的转化率(TF)曲线(产物生成窗口温度)特征与记录的页岩热解图的转化率曲线进行了比较,后者是由多个反应生成的,具有不同的 E-A 值,接近确定的 E-A 趋势。在两个数据集的 TF 曲线值之间发现了重要的异同点。相似之处支持页岩热图最佳拟合所涉及的 E-A 值的分布。造成差异的原因很可能是,记录的页岩热解图中的多个角质一阶和二阶反应非常复杂,而模拟的单个一阶反应则简单明了。这些结果还证明了使用之前描述的 "可变 E-A 热解图拟合方法 "进行多加热速率页岩热解图的有效性,该方法使优化人员能够从无限的 E-A 值范围内选择多种反应。与此相反,Easy%Ro 技术所使用的恒定 A 热图拟合方法的有效性受到了进一步的质疑,因为具有单一 A 值的反应分布不可能代表页岩层中观察到的各种复杂的角质大分子。可变 E-A 烧录曲线拟合法生成的 TF 曲线接近既定的 E-A 趋势,与恒定 A 烧录曲线拟合法生成的 TF 曲线相比,它可能提供更真实的 TF 生成窗口温度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Kerogen Kinetic Distributions and Simulations Provide Insights into Petroleum Transformation Fraction (TF) Profiles of Organic-Rich Shales

Two hundred and fifty single first-order Arrhenius reactions are simulated to generate S2 pyrograms at three heating rates 25, 15, and 5 °C·min−1. The activation energy (E) and pre-exponential factor (A) of the reactions simulated follow a long-established trend of those variable values displayed by shales and kerogens. The characteristics of the transformation fraction (TF) profiles (product generation window temperatures) of the simulated single reactions are compared to the TF profiles of recorded shale pyrograms generated by multiple reactions with different E-A values lying near the defined E-A trend. Important similarities and differences are observed between the TF profile values of the two datasets. The similarities support the spread of E-A values involved in shale pyrogram best fits. The differences are most likely explained by the complexity of the multiple kerogen first-order and second-order reactions contributing to the recorded shale pyrograms versus the simplicity and crispness of the single first-order reactions simulated. The results also justify the validity of using the previously described “variable E-A pyrogram-fitting method” of multi-heating-rate shale pyrograms enabling optimizers to choose multiple reactions from an unlimited range of E-A values. In contrast, further doubt is cast on the validity of the constant-A pyrogram-fitting method used by the Easy%Ro technique, in that a distribution of reactions with a single A value is unlikely to represent the complex variety of kerogen macerals observed in shale formations. TF profiles generated by the variable E-A pyrogram-fitting method lie close to the established E-A trend and are likely to provide more realistic TF generation window temperatures than TF profiles generated by the constant-A pyrogram-fitting method.

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来源期刊
Journal of Earth Science
Journal of Earth Science 地学-地球科学综合
CiteScore
5.50
自引率
12.10%
发文量
128
审稿时长
4.5 months
期刊介绍: Journal of Earth Science (previously known as Journal of China University of Geosciences), issued bimonthly through China University of Geosciences, covers all branches of geology and related technology in the exploration and utilization of earth resources. Founded in 1990 as the Journal of China University of Geosciences, this publication is expanding its breadth of coverage to an international scope. Coverage includes such topics as geology, petrology, mineralogy, ore deposit geology, tectonics, paleontology, stratigraphy, sedimentology, geochemistry, geophysics and environmental sciences. Articles published in recent issues include Tectonics in the Northwestern West Philippine Basin; Creep Damage Characteristics of Soft Rock under Disturbance Loads; Simplicial Indicator Kriging; Tephra Discovered in High Resolution Peat Sediment and Its Indication to Climatic Event. The journal offers discussion of new theories, methods and discoveries; reports on recent achievements in the geosciences; and timely reviews of selected subjects.
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