Multi-scale pore network fusion and upscaling of microporosity using artificial neural network

IF 3.6 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Marine and Petroleum Geology Pub Date : 2025-02-25 DOI:10.1016/j.marpetgeo.2025.107349
Abolfazl Moslemipour , Saeid Sadeghnejad , Frieder Enzmann , Davood Khoozan , Sarah Hupfer , Thorsten Schäfer , Michael Kersten
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Abstract

Digital Rock Physics can significantly enhance our understanding of rock behavior. However, modeling heterogeneous rocks remains challenging because of the trade-off between resolution and field of view. To address this, researchers have developed multi-scale pore network models (PNMs), which integrate PNMs from different scales to create unified multi-scale PNM. Various methodologies exist for merging PNMs from different resolutions, but they often suffer from inaccuracy, high runtime and significant memory consumption, particularly when microporosity is integrated into larger scales. This study introduces a novel fusion and an innovative upscaling approach for efficient multi-scale PNM reconstruction of rocks containing microporosity. Our methods separate resolved and unresolved porosities using different voxel sizes from CT scans at multiple resolutions. Resolved regions have larger voxel sizes, while unresolved areas retain smaller voxel sizes. We extract macro-PNM from the resolved regions and generate stochastic micro-PNM for the unresolved areas. An artificial neural network (ANN), trained on micro-PNM, links micro- and macro-PNMs. The multi-scale PNMs generated using the ANN method had an average permeability of 252 ± 3 mD, closely matching the laboratory-measured permeability of the rock (257 mD). In contrast, the average permeability of multi-scale PNMs reconstructed using the statistical method was significantly higher, at 308 ± 38 mD. Consequently, the ANN-based reconstruction method, owing to the proper connection between scales, improved the accuracy of permeability prediction by approximately 90% compared to the statistical reconstruction method. In the next step, each micro-PNM is upscaled to a base pore based on its effective hydraulic conductance. These base pores are then connected to the macro-PNM using a novel approach. We utilized synchrotron CT images of an Indiana limestone rock at two resolutions as our training dataset. The single- and multi-phase flow analysis of the fused PNM demonstrated excellent agreement with laboratory-measured rock properties. Our upscaling method also reduced runtime by up to 40% (from 312 to 190 CPU-seconds) and memory consumption by approximately 68% (from 25 GB to 8 GB), all without compromising predictive accuracy.

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基于人工神经网络的多尺度孔隙网络融合与微孔隙度提升
数字岩石物理学可以显著提高我们对岩石行为的理解。然而,由于分辨率和视场之间的权衡,非均质岩石的建模仍然具有挑战性。为了解决这一问题,研究人员开发了多尺度孔隙网络模型(PNMs),将不同尺度的孔隙网络模型集成在一起,形成统一的多尺度孔隙网络模型。目前存在多种方法用于合并不同分辨率的pmms,但它们通常存在不准确、运行时间长和内存消耗大的问题,特别是当微孔隙度集成到更大的尺度时。本文介绍了一种新的融合和升级方法,用于含微孔隙岩石的高效多尺度PNM重建。我们的方法在不同分辨率下使用CT扫描的不同体素大小来分离已解决和未解决的孔隙度。已解决的区域具有较大的体素大小,而未解决的区域保留较小的体素大小。我们从已分辨区域提取宏观pnm,并在未分辨区域生成随机微pnm。在微pnm上训练的人工神经网络(ANN)将微观和宏观pnm连接起来。利用人工神经网络方法生成的多尺度pmms的平均渗透率为252±3 mD,与实验室测量的岩石渗透率(257 mD)非常吻合。相比之下,采用统计方法重建的多尺度pmms的平均渗透率明显更高,为308±38 mD。因此,基于神经网络的重建方法由于尺度之间的正确连接,其渗透率预测精度比统计重建方法提高了约90%。在下一步中,每个微pnm根据其有效水力导率被升级为基孔。然后使用一种新颖的方法将这些基础孔连接到宏观pnm。我们利用两种分辨率的印第安纳石灰岩的同步加速器CT图像作为我们的训练数据集。熔融PNM的单相和多相流分析与实验室测量的岩石特性非常吻合。我们的升级方法还减少了高达40%的运行时间(从312到190 cpu秒)和大约68%的内存消耗(从25 GB到8 GB),所有这些都不会影响预测的准确性。
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来源期刊
Marine and Petroleum Geology
Marine and Petroleum Geology 地学-地球科学综合
CiteScore
8.80
自引率
14.30%
发文量
475
审稿时长
63 days
期刊介绍: Marine and Petroleum Geology is the pre-eminent international forum for the exchange of multidisciplinary concepts, interpretations and techniques for all concerned with marine and petroleum geology in industry, government and academia. Rapid bimonthly publication allows early communications of papers or short communications to the geoscience community. Marine and Petroleum Geology is essential reading for geologists, geophysicists and explorationists in industry, government and academia working in the following areas: marine geology; basin analysis and evaluation; organic geochemistry; reserve/resource estimation; seismic stratigraphy; thermal models of basic evolution; sedimentary geology; continental margins; geophysical interpretation; structural geology/tectonics; formation evaluation techniques; well logging.
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