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Estimating permeability from thin sections without reconstruction: Digital rock study of 3D properties from 2D images

机译:在没有重建的情况下估算薄层的渗透率:从2D图像进行3D属性的数字岩石研究

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摘要

We present a new approach for predicting permeability of natural rocks using thin sections. Our approach involves two steps: (1) computing permeability of the thin sections for flow normal to the face, and (2) application of new robust 2D-3D transforms that relate thin section permeability to 3D rock permeability using calibration parameters. We perform step 1 using Lattice-Boltzmann and finite difference schemes, which are memory efficient. We discuss two models to perform step 2. Our two-step approach is fast and efficient, since it does not require reconstruction of the unknown 3D rock using 2D thin section information. We establish the applicability of this new approach using a dataset comprised of LBM-computed permeability of rock samples from various geologic formations, including Fontainebleau sandstone, Berea sandstone, Bituminous sand, and Grosmont carbonate. We find that for sandstones our approach predicts fairly accurate permeability with little calibration. Predicting permeability of carbonates from thin sections is more challenging due to microstructural complexity thus model parameters require more calibration. For general workflow, we propose to first calibrate the proposed models using the available 3D information on the rock microstructure (from microCT, SEM, etc.) and then predict the permeability for rocks from the same geological formation for which only 2D thin sections are available.
机译:我们提出了一种使用薄截面来预测天然岩石渗透率的新方法。我们的方法涉及两个步骤:(1)计算薄壁的渗透率以垂直于工作面流动;(2)应用新的鲁棒2D-3D转换,该转换使用校准参数将薄层渗透率与3D岩石渗透率相关联。我们使用Lattice-Boltzmann和有限差分方案执行第1步,这是高效存储的。我们讨论了执行第2步的两个模型。我们的两步方法是快速且高效的,因为它不需要使用2D薄截面信息来重建未知的3D岩石。我们使用由LBM计算的各种地质​​构造(包括枫丹白露砂岩,Berea砂岩,沥青砂和Grosmont碳酸盐岩)的岩石样品的渗透率组成的数据集,来建立这种新方法的适用性。我们发现,对于砂岩,我们的方法可以预测出相当准确的渗透率,而几乎不需要校准。由于微观结构的复杂性,预测薄层碳酸盐岩的渗透率更具挑战性,因此模型参数需要更多的校准。对于一般的工作流程,我们建议首先使用岩石微观结构上的可用3D信息(来自microCT,SEM等)来对提议的模型进行校准,然后预测只有2D薄截面可用的同一地质构造的岩石渗透率。

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