首页> 外文会议>SPWLA annual logging symposium >DETERMINATION OF FORMATION ORGANIC CARBON CONTENT USING A NEW NEUTRON-INDUCED GAMMA RAY SPECTROSCOPY SERVICE THAT DIRECTLY MEASURES CARBON
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DETERMINATION OF FORMATION ORGANIC CARBON CONTENT USING A NEW NEUTRON-INDUCED GAMMA RAY SPECTROSCOPY SERVICE THAT DIRECTLY MEASURES CARBON

机译:使用新的中子诱导的γ射线光谱服务测定形成有机碳含量,直接测量碳

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Over the past few decades, many techniques have been developed for the log evaluation of organic-rich rocks (ORR). More recently, ORR have gained economic interest across the globe, not only as the source rocks for conventional reserves, but also as potential reservoirs themselves. Quantifying total organic carbon (TOC) and the complex mineralogy of these rocks are two key components for a robust characterization. A number of well-log-derived TOC indicators based on measurements such as gamma ray, spectral gamma ray, resistivity, density, sonic, neutron, and nuclear magnetic resonance (NMR) have been developed over the years with different levels of success depending on the specific ORR and where it occurs within a basin. An accurate TOC estimation faces two main challenges: 1) the necessity for a correlation of log data with core to utilize the most representative model and 2) extensive log interpretation. The process of an empirically derived TOC has been hindered by the lack of a consistent direct organic carbon measurement. The introduction of a new neutron-induced capture and inelastic gamma ray spectroscopy tool using a very high-resolution scintillator and a new type of pulsed neutron generator allows us to measure new elements which, in turn, increases our ability to properly interpret lithologically complex formations. In addition to measuring elements derived from capture spectroscopy, this new service is capable of measuring reliable inelastic yields, including carbon, at reasonable logging speeds. This carbon measurement allows the calculation of a stand-alone quantitative TOC value that does not require local calibrations or multitool interpretation. This is possible because of the successful combination of capture and inelastic gamma ray spectra. Inorganic carbon in carbonate is estimated by using other elements from this logging tool (Ca, Mg, Mn, Fe) to estimate total carbonate, and this value is subtracted from the measured total carbon to give TOC.
机译:在过去的几十年中,已经开发了许多技术用于有机富岩石的日志评估(ORR)。最近,ORR在全球上获得了经济兴趣,不仅是传统储备的源岩,而且作为潜在的水库本身。量化总有机碳(TOC)和这些岩石的复合矿物是稳健特性的两个关键组分。多年来,多年来,多年来,多年来,基于伽马射线,光谱伽马射线,电阻率,密度,声音,中子和核磁共振(NMR)的许多良好的对数衍生的TOC指标已经开发出来,这取决于不同程度的成功水平特定的ORR和它在盆内发生的地方。准确的TOC估计面临的两个主要挑战:1)必须使用核心的日志数据与利用最具代表性模型和2)广泛的日志解释的必要性。缺乏一致直接有机碳测量的凭经质衍生的TOC的方法已经受到阻碍。使用非常高分辨率的闪烁体和新型脉冲中子发生器的新中子诱导的捕获和无弹性伽马射线光谱工具允许我们测量新的元素,这反过来又增加了我们正确解释了岩性复杂地层的能力。除了从捕获光谱衍生的测量元素之外,这种新的服务能够在合理的测井速度下测量可靠的无弹性产量,包括碳。该碳测量允许计算不需要局部校准或多池解释的单独定量TOC值。这是可能的,因为捕获和非弹性伽马射线光谱的成功组合。通过使用来自该测井工具(Ca,Mg,Mn,Fe)的其他元素来估计碳酸盐中的无机碳以估计总碳酸盐,并且从测量的总碳中减去该值以提供TOC。

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