A Rapid Reconstruction Method of 3D Digital Rock with Strong Pore Connectivity

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS pure and applied geophysics Pub Date : 2024-04-10 DOI:10.1007/s00024-024-03473-5
Weichao Yan, Naser Golsanami, Huilin Xing, Sanzhong Li, Peng Chi
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Abstract

As a technique capable of replacing laboratory experiments, a large number of digital rock simulations have been widely used for the characterization of reservoir petrophysical parameters. For conditions with less coring data, rapid reconstruction of three-dimensional (3D) digital rocks using two-dimensional (2D) pore structure images is an important prerequisite for the accurate calculation of petrophysical parameters. However, the conventional digital rock rapid reconstruction method with poor pore connectivity leads to the erroneous evaluation of key reservoir rock parameters (e.g., permeability and resistivity ). In this study, we used the sequential indicator simulation method as the base data and combined the erosion operation and expansion operation in mathematical morphology to realize the rapid construction of 3D digital rock models with strong pore connectivity . The accuracy of the digital rock model reconstructed by the new method was verified by comparing with the permeability and electrical properties obtained by the CT-based method, sequential indicator simulation method, multi-point statistical method, process-based method, and deep leaning method. This study overcomes the shortcomings of the sequential indicator simulation digital rock reconstruction method in terms of small pore radius and poor pore connectivity, improves the permeability of constructing 3D digital rocks, and lays the foundation for accurate and rapid analysis of petrophysical properties.

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具有强孔隙连通性的三维数字岩石快速重建方法
作为一种能够替代实验室实验的技术,大量数字岩石模拟已被广泛应用于储层岩石物理参数的表征。在取芯数据较少的条件下,利用二维孔隙结构图像快速重建三维(3D)数字岩石是准确计算岩石物理参数的重要前提。然而,传统的数字岩石快速重建方法孔隙连通性差,导致对储层岩石关键参数(如渗透率和电阻率)的错误评估。本研究以顺序指标模拟方法为基础数据,结合数学形态学中的侵蚀运算和膨胀运算,实现了孔隙连通性强的三维数字岩石模型的快速构建。通过与基于 CT 的方法、顺序指标模拟方法、多点统计方法、基于过程的方法和深部倾斜方法得到的渗透率和电性进行比较,验证了新方法重建的数字岩石模型的准确性。该研究克服了顺序指示器模拟数字岩石重建方法孔隙半径小、孔隙连通性差的缺点,提高了构建三维数字岩石的渗透性,为准确、快速地分析岩石物性奠定了基础。
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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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