Department of Earth Sciences, Khalifa University of Science and Technology, Abu Dhabi, United Arab Emirates.
Department of Mathematics, Khalifa University of Science and Technology, Abu Dhabi, United Arab Emirates.
PLoS One. 2024 Feb 8;19(2):e0295192. doi: 10.1371/journal.pone.0295192. eCollection 2024.
This study presents a comprehensive analysis of rock properties for a selected group of six carbonate reservoir rock samples revealing complex structures at various length scales. Experimental laboratory methods as well as image analysis techniques were conducted in this study to characterize the macro- and micro-pores in mud- and grain-dominated limestones samples from the Upper Jurassic Arab Formation (Arab D member). Mercury Injection Capillary Pressure (MICP), porosimeter, and permeameter lab measurements were employed to assess the pore network heterogeneity and complexity. In addition, a multiscale rock imaging approach was implemented to detect grain and pore phases at several length scales using Thin Sections (TS), Scanning Electron Microscopy (SEM), Focused Ion Beam Scanning Electron Microscopy (FIB-SEM), as well as 3D X-ray Computed Tomography (CT), and micro-computed tomography images (MCT). Furthermore, the multifractal analysis method was applied on the MICP and FIB-SEM to characterize quantitatively the heterogeneity of the pores in the studied samples. Heterogeneous samples 3R, 4M, 5W, and 6M display the highest non-uniformity degree Δα values, falling within the range of [1.21, 1.39] based on FIB-SEM images. Samples 1G, 2R, 3R, and 5W exhibit more heterogeneous pore structure, with Δα values ranging from 0.73 to 1.49 based on the MICP experiments. The results and findings confirm the effectiveness of multifractal parameters Δα and the asymmetry degree in the vertical axis Δf(α) in quantifying and characterizing rock heterogeneity.
本研究对六组选定的碳酸盐储层岩石样本的岩石特性进行了全面分析,揭示了不同长度尺度下的复杂结构。本研究采用了实验实验室方法和图像分析技术,对来自上侏罗统阿拉伯组(Arab D 成员)的泥质和颗粒主导的灰岩样品中的宏-微观孔隙进行了特征描述。采用压汞毛细管压力(MICP)、孔隙度计和渗透率计实验室测量来评估孔隙网络的非均质性和复杂性。此外,还采用了多尺度岩石成像方法,使用薄片(TS)、扫描电子显微镜(SEM)、聚焦离子束扫描电子显微镜(FIB-SEM)以及 3D X 射线计算机断层扫描(CT)和微计算机断层扫描图像(MCT),在几个长度尺度上检测颗粒和孔隙相。此外,还应用多重分形分析方法对 MICP 和 FIB-SEM 进行分析,以定量表征研究样品中孔隙的非均质性。非均质样品 3R、4M、5W 和 6M 显示出最高的非均匀度Δα 值,根据 FIB-SEM 图像,其值在[1.21,1.39]范围内。样品 1G、2R、3R 和 5W 表现出更不均匀的孔隙结构,根据 MICP 实验,Δα 值在 0.73 到 1.49 之间。研究结果和发现证实了多重分形参数Δα 和垂直轴Δf(α)的不对称度在量化和表征岩石非均质性方面的有效性。