用校正后的岩石热解数据检测重质沥青污染

M. Hemmati, Y. Ahmadi
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引用次数: 0

摘要

岩石热解是石油地质学家广泛应用的一种评价烃源岩特征和获取地球化学参数的热方法。然而,在特殊情况下,由于存在误解和误用,可能导致使用岩石热解评价有机质性质的错误结论,S2(石油潜力)与TOC(总有机碳)的交叉图是一个可用的工具,可以帮助更好地解释。该图可作为地球化学参数精度的判据,并对S2、HI(氢指数)、干酪根类型、矿物基质对烃的吸附等指标进行校正。此外,本文还演示了一种基于图的沥青或碳氢化合物污染检测方法。基于对伊朗石油地质中Garau组可能为烃源岩的认识,利用rock - eval VI热解和Leco碳分析仪对伊朗西南部高扎格罗斯地区Aligudarz地区Lurestan省不同露头剖面的样品进行了地球化学研究。将数据绘制成S2与TOC的交叉图,并确定回归方程,是确定S2和HI参数真实值和测量沥青或烃污染的最佳方法。烃污染使地球化学数据不可靠,在两个研究点不现实地增加了S2和HI,降低了Tmax值,降低了烃源岩样品有机质或干酪根的热成熟度水平。为了跳过污染的影响,获得真实的地球化学参数,必须去掉图的y截距。Garau组富有机质相污染的原因是重质沥青与有机质相的黏附作用,这是由于碳、氢离子之间的共价键。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Detection of heavy bitumen contaminations with using corrected Rock-Eval pyrolysis data
The Rock-Eval pyrolysis is a thermal method that is widely used by the petroleum geologist for evaluation of source rock characteristics and obtain geochemistry parameters. However, there are misconceptions and misuse in exceptional cases which could lead to erroneous conclusions in using Rock-Eval pyrolysis to evaluate properties of the organic matter, a cross-plot of S2 (petroleum potential) versus TOC (total organic carbon) is an usable tool which can facilitate better interpretations. The graph can apply as a criterion accuracy of geochemistry parameters, and provides the correction for S2, HI (hydrogen index), kerogen type, and measuring the adsorption of hydrocarbon by the mineral matrix. In addition, this article demonstrates a manner based on the graph to detect bitumen or hydrocarbon contaminations. Based on our knowledge about the Garau Formation as a possible source rock in petroleum geology of Iran, a geochemical study using Rock-Eval VI pyrolysis and Leco Carbon Analyzer has been conducted on samples from different outcrop sections in Lurestan province, Aligudarz region, from South-West of Iran, High Zagros. Plotting the data on a cross plot of S2 versus TOC, and determining the regression equation is the best method for determining the real values of S2 and HI parameters and measuring the contamination by bitumen or hydrocarbon. Hydrocarbon contaminations makes geochemistry data unreliable, as unrealistically increase S2 and HI, lower Tmax values, and reduce the thermal maturity level of organic matters or kerogen of source rock samples in two study locations. For skipping the effect of contamination and obtaining the real geochemistry parameters, the y-intercept of the graphs must be removed. The cause of contamination in organic rich facies of the Garau Formation is the adhesion of heavy bitumen to organic facies which is due to the covalent bonds between carbon and hydrogen ions.
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