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Mapping permeability in low-resolution micro-CT images: A multiscale statistical approach

机译:低分辨率微CT图像中的渗透率映射:一种多尺度统计方法

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摘要

We investigate the possibility of predicting permeability in low-resolution X-ray microcomputed tomography (mu CT). Lower-resolution whole core images give greater sample coverage and are therefore more representative of heterogeneous systems; however, the lower resolution causes connecting pore throats to be represented by intermediate gray scale values and limits information on pore system geometry, rendering such images inadequate for direct permeability simulation. We present an imaging and computation workflow aimed at predicting absolute permeability for sample volumes that are too large to allow direct computation. The workflow involves computing permeability from high-resolution mu CT images, along with a series of rock characteristics (notably open pore fraction, pore size, and formation factor) from spatially registered low-resolution images. Multiple linear regression models correlating permeability to rock characteristics provide a means of predicting and mapping permeability variations in larger scale low-resolution images. Results show excellent agreement between permeability predictions made from 16 and 64 mu m/voxel images of 25 mm diameter 80 mm tall core samples of heterogeneous sandstone for which 5 mu m/voxel resolution is required to compute permeability directly. The statistical model used at the lowest resolution of 64 mu m/voxel (similar to typical whole core image resolutions) includes open pore fraction and formation factor as predictor characteristics. Although binarized images at this resolution do not completely capture the pore system, we infer that these characteristics implicitly contain information about the critical fluid flow pathways. Three-dimensional permeability mapping in larger-scale lower resolution images by means of statistical predictions provides input data for subsequent permeability upscaling and the computation of effective permeability at the core scale.
机译:我们调查在低分辨率X射线计算机断层扫描(μCT)中预测渗透率的可能性。较低分辨率的全核心图像会提供更大的样本覆盖率,因此更能代表异构系统。但是,较低的分辨率会导致连接孔喉由中间灰度值表示,并限制了有关孔系统几何形状的信息,从而使此类图像不足以进行直接渗透率模拟。我们提出了一种成像和计算工作流程,旨在预测太大而无法直接计算的样本量的绝对渗透率。该工作流程涉及从高分辨率mu CT图像计算渗透率,以及从空间配准的低分辨率图像计算一系列岩石特征(尤其是开孔分数,孔径和形成因子)。将渗透率与岩石特征相关联的多个线性回归模型提供了一种预测和映射大规模低分辨率图像中渗透率变化的方法。结果表明,由25毫米直径,80毫米高的非均质砂岩岩心样品的16和64μm / voxel图像进行的渗透率预测之间具有极好的一致性,而要直接计算渗透率,需要5μm / voxel分辨率。在最低分辨率为64μm / voxel(类似于典型的整个核心图像分辨率)下使用的统计模型包括开孔分数和形成因子作为预测特征。尽管在此分辨率下的二值化图像不能完全捕获孔隙系统,但我们推断这些特征隐含了有关关键流体流动路径的信息。借助统计预测,在较大尺寸低分辨率图像中进行三维渗透率映射可为后续渗透率放大和岩心尺度有效渗透率的计算提供输入数据。

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