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Comparison of low-field NMR and microfocus X-ray computed tomography in fractal characterization of pores in artificial cores

机译:低场核磁共振和微焦点X射线计算机断层扫描在人造岩心孔隙分形表征中的比较

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摘要

Studying the pore structure is very important for better understanding the characteristics of fluids storage and transport in rock reservoirs. To investigate the better way to characterize complex pore structures of rock reservoir, three artificial core samples with different permeabilities were investigated by Micro X-ray computed tomography (Micro-CT) and Nuclear Magnetic Resonance (NMR). A method for quantifying NMR pore structure is proposed based on the pore geometry derived from Micro-CT. The Pore Size/volume Distribution (PSD) from Micro-CT and NMR was compared. Moreover, some macroscopic physical properties of the cores were explained at the micro-scale based on the fractal analysis. Our results show that Micro-CT is a reliable and convenient way to interpret the NMR T-2 spectrum into real PSD for some brittle materials. The difference between 2D and 3D box-counting fractal dimensions of pores in artificial cores is less than one. The fractal dimensions of pores demonstrate a good negative correlation with the permeability. Moreover, the calculated fractal dimensions prove the existence of multiple fractal structure in artificial cores based on the NMR measurement. The fractal properties of PSD are mainly governed by the large pores in the tested cores. It was also found that the complexity of pore surface and fine pore structure has significant influence on heterogeneity. Finally, Micro-CT is proved to be ineffective in describing the fractal characteristics of a wide range of pore sizes due to limitation of resolution, which could be achieved by NMR more easily.
机译:为了更好地理解岩石储层中流体的储运特性,研究孔隙结构非常重要。为了研究更好的表征岩石储层复杂孔隙结构的方法,通过微X射线计算机断层扫描(Micro-CT)和核磁共振(NMR)研究了三种渗透率不同的人工岩心样品。提出了一种基于Micro-CT的孔几何定量NMR孔结构的方法。比较了来自Micro-CT和NMR的孔径/体积分布(PSD)。此外,基于分形分析,从微观角度解释了岩心的一些宏观物理性质。我们的结果表明,对于某些脆性材料,Micro-CT是将NMR T-2谱图解释为实际PSD的可靠且便捷的方法。人工岩心中孔隙的2D和3D盒计数分形维数之差小于一。孔隙的分形维数与渗透率具有良好的负相关性。此外,计算的分形维数证明了基于核磁共振测量的人工岩心中多重分形结构的存在。 PSD的分形特性主要受测试岩心中大孔的支配。还发现孔表面的复杂性和细孔结构对非均质性有显着影响。最后,事实证明,由于分辨率的限制,Micro-CT在描述大范围孔径的分形特征方面无效,而这可以通过NMR更容易地实现。

著录项

  • 来源
    《Fuel》 |2017年第15期|217-226|共10页
  • 作者单位

    China Univ Min & Technol, State Key Lab Coal Resources & Safe Min, Beijing 100083, Peoples R China|China Univ Min & Technol, Coll Resources & Safety Engn, Beijing 100083, Peoples R China|China Univ Min & Technol, Beijing Key Lab Precise Min Intergrown Energy & R, Beijing 100083, Peoples R China;

    China Univ Min & Technol, Coll Resources & Safety Engn, Beijing 100083, Peoples R China|China Univ Min & Technol, Beijing Key Lab Precise Min Intergrown Energy & R, Beijing 100083, Peoples R China;

    Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China;

    Univ Queensland, Sch Mech & Min Engn, St Lucia, Qld 4072, Australia;

    Univ Queensland, Sch Mech & Min Engn, St Lucia, Qld 4072, Australia;

    China Univ Min & Technol, Coll Resources & Safety Engn, Beijing 100083, Peoples R China|China Univ Min & Technol, Beijing Key Lab Precise Min Intergrown Energy & R, Beijing 100083, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Artificial core; Pore structure; NMR; Micro-CT; Digital core; Fractal dimension;

    机译:人工岩心孔结构核磁共振Micro-CT数字岩心分形维数;

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