用数字岩石方法对曲采坝页岩有机质含量进行一致性评价

M. Abouelresh, M. Khodja, Rizwanullah Husseini, H. Al-Mukainah, Abdelwahab Ali
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引用次数: 1

摘要

非常规油气资源作为一种潜在的能源,越来越受到人们的关注。这反映在正在进行的旨在更好地了解潜在非常规储层的研究中。在这篇文章中,我们描述了一项针对沙特阿拉伯富有机质页岩的研究,即Qusaiba页岩。该研究的主要目的是利用经过实验室测量验证的数字岩石方法,量化有机质含量、矿物含量和孔隙度。岩塞选自富有机质的曲赛坝页岩的全岩心。首先使用高分辨率μ CT扫描对岩心桥塞进行数字化,并对获得的三维模型进行分割,以分离总有机含量(TOC)体积、岩石基质和孔隙网络。进行x射线衍射(XRD), x射线荧光(XRF)和定量扫描电子显微镜(SEM)分析以确定元素和矿物组成。为了表征页岩的孔隙度,样品还需要进行SEM成像和核磁共振(NMR)分析。在此基础上进行了数值放大,并对数值结果和实验结果进行了比较。岩石学和矿物学分析表明,曲赛坝页岩样品的主要矿物成分为二氧化硅、长石、云母、粘土和黄铁矿。扫描电镜成像显示,在纳米尺度上,样品具有各种孔隙类型,大小和形态的特征。孔隙分粒间型和有机质型两种类型,其中粒间型孔隙占主导地位。碎屑矿物颗粒的压实和水平排列控制着粒间孔隙度的发育,而有机颗粒的分布及其成熟度是控制有机孔隙度形成的关键因素。整合SEM图像,高分辨率x射线扫描和核磁共振测量提供了用于定量确定样品的矿物和有机含量的信息。初步结果表明,升级后的基于岩石的数字估计与实验测量结果一致。本研究的主要贡献是基于数字岩石物理(DRP)的经济实惠的表征,表征了代表沙特阿拉伯潜在页岩气储层的样品的有机含量、矿物含量和孔隙网络结构,与实验室测量结果一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Consistent Evaluation of the Organic Content of the Qusaiba Shale Using Digital-Rock Methodology
Unconventional hydrocarbon resources continue to engender increasing attention as potential energy sources. This is reflected in the ongoing research aiming at gaining a better understanding of potential unconventional reservoirs. In this note, we describe a study focused on an organic-rich, potential gas-producer shale from Saudi Arabia, namely the Qusaiba Shale. The study aims, in particular, to quantify organic matter content, mineral content, and porosity using digital-rock methodology validated by laboratory measurements. Rock plugs are selected from whole cores representative of the organic-rich, Qusaiba Shale. The core plugs are first digitized using high-resolution μ CT scan and the obtained 3D models are segmented to separate the total organic content (TOC) volume, rock matrix, and pore network. X-ray diffraction (XRD), X-ray fluorescence (XRF), and quantitative scanning electron microscopy (SEM) analyses are undertaken to determine elemental and mineralogical composition. To characterize porosity at a level adequate for shale, the samples also undergo SEM imaging, as well as nuclear magnetic resonance (NMR) analysis. Subsequently, numerical upscaling is applied and comparison of numerical and experimental results is performed. Petrography and mineralogy analyses show that the major mineral components of the Qusaiba Shale samples are silica, feldspars, mica, clay, and pyrite. SEM imaging reveals that, at the nanoscale, the samples are characterized by a variety of pore types, sizes, and morphologies. Porosity comes in two types: intergranular and organic, with intergranular porosity being the dominant type. Compaction and horizontal alignment of the detrital mineral grains control the development of intergranular porosity while the distribution of organic particles, as well as their maturity, are the key factors controlling the formation of organic porosity. Integrating SEM images, high-resolution X-ray scans, and NMR measurements provides the information utilized to quantitatively determine the mineral and organic contents of the samples. Preliminary results exhibit a consistent agreement between the upscaled digital-rock-based estimates and the experimental measurements. The main contribution of this study is an affordable, Digital Rock Physics (DRP)-based characterization of the organic content, mineral content, and pore-network structure of samples representative of Saudi Arabia's potential shale gas reservoirs that is consistent with laboratory measurements.
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