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NMR relaxometry a new approach to detect geochemical properties of organic matter in tight shales

机译:核磁共振弛豫法是一种检测致密页岩中有机物地球化学性质的新方法

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摘要

Understanding organic matter properties in terms of maturity and production potential are crucial for the initial assessment of unconventional plays. This is important since the amount of hydrocarbon that can be generated is a function of organic matter type and content in the formation and its thermal maturity. The complexity of shale plays in terms of constituent components has demonstrated that new analytical methods should be acquired to better understand hydrocarbon generation processes. In this study, a few samples from the upper and lower members of the Bakken Formation in the USA were selected from different depths and maturity levels. The samples were analyzed by a high frequency (22 MHz) nuclear magnetic resonance (NMR relaxometry) equipment, followed by Rock-Eval pyrolysis (using the Basic/Bulk-Rock method for all samples and a multi-heating rate method, MHR, for the two least mature samples) and bitumen reflectance evaluations. Results showed NMR can detect different hydrogen populations within the samples and distinguish among phases, such as solid organic matter, hydrocarbons (mobile oil), and water by T-1-T-2 mapping. We were also able to relate different identified areas on NMR T-1-T-2 maps to geochemical parameters of the organic matter obtained from Rock-Eval pyrolysis (such as S1, S2, and HI) and with thermal maturity (vitrinite reflectance- equivalent).
机译:从成熟度和生产潜力的角度了解有机物特性对于非常规油气的初步评估至关重要。这很重要,因为可以产生的碳氢化合物的量是有机质类型,地层含量及其热成熟度的函数。页岩气在组成成分方面的复杂性表明,应获取新的分析方法,以更好地理解烃的生成过程。在这项研究中,从美国的Bakken地层的上,下部分中选出了一些不同深度和成熟度的样品。样品先通过高频(22 MHz)核磁共振(NMR弛豫法)设备进行分析,然后进行Rock-Eval热解(对所有样品使用Basic / Bulk-Rock方法,然后采用多重加热速率方法MHR)进行分析。两个最不成熟的样品)和沥青反射率评估。结果表明,NMR可以检测样品中不同的氢种群,并通过T-1-T-2绘图区分出相,例如固体有机物,烃(流动油)和水。我们还能够将NMR T-1-T-2图谱上的不同识别区域与通过岩石-Eval热解(例如S1,S2和HI)获得的有机物的地球化学参数相关联,并具有热成熟度(镜质体反射率-当量)。

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