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POROSITY AND PERMEABILITY ANALYSIS ON NANOSCALE FIB-SEM 3D IMAGING OF SHALE ROCK

机译:页岩岩纳米尺度FIB-SEM 3D成像的孔隙度和渗透性分析

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As oil and gas production from conventional reservoirs is declining and oil price is going up,unconventional mudstone reservoirs(“shale-gas”) are becoming more important. However,while their characterization is of utmost importance for production planning, these low permeability rocks are very challenging to characterize due to their complex nano-scale pores and mineral structure.3D imaging is a critical tool in the visualization, analysis and modeling of these type of reservoirs. In this study,FIB-SEM(Focused Ion Beam - Scanning Electron Microscopy) 3D imaging at 5nm pixel resolution was used to study porosity,connectivity,and to model permeability of a mudstone core sample extracted from a production well in North America.With 3D reconstruction,extraordinary detail of the pore space in both the mineral and organic matter phases can be visualized and analyzed.Advanced image analysis algorithms were used to extract volumes of the different phases and to compare these with the physical laboratory experiments of porosity and permeability.Special focus was placed on the impact of pore space in the organic matter.These pores tend to be larger than the other pore types.The impact of segmentation procedure on porosity calculation was systematically studied. Segmented FIB-SEM images are used as the input to the Stokes flow solver to simulate viscous fluid flow through the rock.The simulation results can be compared with physical laboratory experiments. In addition to analysis of mudstone samples,the workflow proposed by this study is potentially applicable to a wide range of core sample and more general porous material analysis.
机译:随着传统水库的石油和天然气产量正在下降,油价上涨,非常规泥岩水库(“页岩气”)变得越来越重要。然而,虽然它们的表征对于生产计划至关重要,但这些低渗透性岩石是由于它们的复杂纳米尺度孔隙和矿物结构的表征非常具有挑战性.3D成像是这些类型的可视化,分析和建模中的关键工具水库。在该研究中,使用以5nm像素分辨率的FIB-SEM(聚焦离子束扫描电子显微镜)3D成像用于研究孔隙率,连通性,以及从北美生产井中提取的泥石核心样品的模型渗透性。3D矿物质和有机物相中孔隙空间的重建,可以进行可视化和分析孔隙空间的特殊细节.Advanced图像分析算法用于提取不同阶段的体积,并将这些与孔隙率和渗透性的物理实验室实验进行比较。重点放在有机物质中孔隙空间的影响。这些孔趋于大于其他孔隙类型。系统地研究了分段过程对孔隙率计算的影响。分段的FIB-SEM图像用作STOKES流动求解器的输入,以模拟粘性流体流过岩石。可以将仿真结果与物理实验室实验进行比较。除了对泥岩样品的分析之外,本研究提出的工作流程可能适用于各种核心样品和更通用的多孔材料分析。

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