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首页> 外文期刊>Energy & fuels >Rapid Analysis of Kerogen Hydrogen-to-Carbon Ratios in Shale and Mudrocks by Laser-Induced Breakdown Spectroscopy
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Rapid Analysis of Kerogen Hydrogen-to-Carbon Ratios in Shale and Mudrocks by Laser-Induced Breakdown Spectroscopy

机译:利用激光诱导击穿光谱法快速分析页岩和泥浆中的干酪根氢碳比

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摘要

Evaluation of organic matter quality in petroleum source and reservoir rocks is vital for economic, drilling, and production decisions. However, current methods for assessing kerogen quality in shales and mudrocks are either time-intensive and undesirable from a health, safety, and waste-disposal standpoint or indirect measurements of the factors of greatest interest and utility (e.g., kerogen hydrogen content). We present a new approach using laser-induced breakdown spectroscopy (LIBS) to both directly and quickly measure kerogen hydrogen-to-carbon elemental ratios in shales and mudrocks, providing a rapid means of assessing kerogen quality and thermal maturity with minimal sample processing. Elemental spectral intensities, including hydrogen and carbon, were monitored during LIBS measurements by optical emission spectroscopy, following ablation of a small portion of rock. Changes in the elemental intensities in the spectra over the course of LIBS measurements were then related to H/C ratios determined on isolated kerogens from the rock samples using multivariate analysis. Predicted kerogen H/C ratios from the LIBS measurements of whole rock samples were well-correlated (R-2 = 0.99) to values determined for kerogen isolates measured by elemental analysis. These results demonstrate that LIBS is a promising method for examining kerogen quality and thermal maturity in source and reservoir rocks. Because LIBS does not require samples to be pulverized and can be conducted on sub-millimeter scales, this approach will also allow for highly localized, spatially resolved measurements on heterogeneous geologic samples.
机译:评估石油源岩和储层岩石中的有机物质量对于经济,钻探和生产决策至关重要。但是,目前评估页岩和泥岩中干酪根质量的方法要么时间密集,要么从健康,安全和废物处置的角度出发,或者对最感兴趣和最有用的因素(例如干酪根氢含量)进行间接测量都是不可取的。我们提出了一种使用激光诱导击穿光谱法(LIBS)的新方法,可以直接,快速地测量页岩和泥岩中的干酪根氢碳比,从而以最少的样品处理提供了一种快速评估干酪根质量和热成熟度的方法。在消融一小块岩石后,通过光发射光谱法在LIBS测量期间监测元素光谱强度,包括氢和碳。然后,通过多变量分析,在LIBS测量过程中,光谱元素强度的变化与从岩石样品中分离出的干酪根确定的H / C比有关。从整个岩石样品的LIBS测量值预测的干酪根H / C比值与通过元素分析测定的干酪根分离物确定的值具有良好的相关性(R-2 = 0.99)。这些结果表明,LIBS是检查源岩和储层岩石中干酪根质量和热成熟度的一种有前途的方法。因为LIBS不需要将样品粉碎,并且可以在亚毫米规模上进行,所以这种方法还将允许对异质地质样品进行高度局部化,空间分辨的测量。

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  • 来源
    《Energy & fuels》 |2015年第novaadeca期|6999-7004|共6页
  • 作者单位

    US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA;

    Ingrain Inc, Houston, TX 77027 USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
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