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Multi-Frequency NMR and TGA Characterization of TOC in Shales

机译:Shales中TOC的多频NMR和TGA表征

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The production of unconventional shale assets depends on an understanding of pore structure,fluid content and distribution within the reservoir rock. The nanometer scale pores and range of hydrocarbon types(mobile vs. immobile hydrocarbons)present in shale reservoirs lead to difficulty in using conventional petrophysical measurements to produce quantitative values for important parameters such as porosity,fluid content or saturation. Many existing techniques can be used to characterize these materials,but it can be useful to combine multiple standard measurements to provide a more quantitative understanding of rock properties. T1-T2 NMR relaxation maps can provide insight into the fluids present in the shales,and measurements of the total organic content(TOC)provide an estimate of the amount of organic material. Since the NMR signal in shales is largely due to the hydrocarbons in place,it is probable that magnetic resonance should provide a direct probe of the amount and type of hydrocarbon types in a shale sample. Further clarification can be provided by the addition of thermal analysis methods combined with mass spectroscopy. In this work,we present experimental results showing not only a direct correlation between TOC and T1/T2 ratio as measured by 2D NMR,but also a frequency dependence of this relationship. We further correlate these results with compositional data provided by thermogravimetric analysis with mass spectroscopy(TGA-MS). Our measurements cover several different shale types and span a wide range of TOC. 2D NMR spectra were obtained at multiple frequencies on crushed shale samples that were exposed to the key temperatures indicated in the TGA results. The results helped to correlate compositional changes to regions of the 2D relaxation maps,potentially providing a method for determining the amount of mobile and immobile hydrocarbons that constitute the total organic carbon content in shale.
机译:非传统页岩资产的生产取决于对储层岩石内的孔隙结构,流体含量和分布的理解。在页岩储层中存在的纳米垢孔和范围存在于页岩储层中的烃类(移动与固定烃类)导致使用常规岩石物理测量来产生重要参数的定量值,例如孔隙率,流体含量或饱和度。许多现有技术可用于表征这些材料,但是将多个标准测量结果结合以提供对岩石特性的更加定量了解。 T1-T2 NMR弛豫图可以提供进入所存在的流体中存在的流体,并且总有机含量(TOC)的测量提供了有机材料量的估计。由于HALES中的NMR信号很大程度上是由于烃的适当位置,因此磁共振应该提供页岩样品中的烃类别的量和烃类类型的直接探针。通过添加热分析方法可以提供进一步的澄清方法,与质谱相结合。在这项工作中,我们呈现实验结果,不仅显示通过2D NMR测量的TOC和T1 / T2比率之间的直接相关性,而且表明这种关系的频率依赖性。我们进一步将这些结果与具有质谱(TGA-MS)的热重分析提供的ThermoGrimetric分析提供的组成数据相关联。我们的测量涵盖了几种不同的页岩类型,跨越了各种TOC。在多个频率上获得2D NMR光谱,粉碎的页岩样品上暴露于TGA结果中所示的关键温度。结果有助于将组成变化与2D弛豫图的区域相关,潜在地提供用于确定构成页岩中总有机碳含量的移动和固定烃量的方法。

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