Investigating The Permeability Prediction Using Geometric Properties of Micro Computed Tomography Images by Linear Regression Models

M. Ashrafi, S. A. Tabatabaei-Nejad, E. Khodapanah
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Abstract

Challenges on rock absolute permeability prediction from tiny sample when laboratory apparatus is not applicable and without pore network modelling is remarkable. This prediction using the characterization of micro-computed tomography images have been studied in this paper. Twenty series of 2D micro computed tomography rock binary images have been collected, each of them was considered as a 3D binary image. Their geometric measures in 2D and 3D for measuring image properties have been considered using Minkowski functionals and available functions, developing a regression model, absolute permeabilities have been evaluated. Some 2D and 3D geometric properties are considered. The area, the perimeter and the 2D Euler number are 2D binary images properties. The volume, the surface area, the mean breadth also known as integral of the mean curvature, and the 3D Euler Number are 3D binary images properties. Porosity and number of objects also have been considered as parameters of a regression model.To perform linear regression, twenty-four parameters were evaluated and some of them were chosen to be used. An equation is proposed based on the extensive study conducted which can predict rock permeability. This equation has two sets of parameter coefficients, one set predicts high permeability rocks (above two Darcy) and the other for low and medium permeability (less than two Darcy) which can be used for carbonated rock. Average absolute relative error for conducted cases is 0.06.
基于线性回归模型的微计算机断层图像几何性质渗透率预测研究
在实验室设备不适用且没有孔隙网络模型的情况下,小样本岩石绝对渗透率预测面临着巨大的挑战。本文研究了利用微计算机断层扫描图像的特征进行预测。采集了20组二维微计算机断层岩石二值图像,将每组图像视为三维二值图像。利用Minkowski函数和可用函数,考虑了测量图像属性的二维和三维几何测量,建立了回归模型,并对绝对渗透率进行了评估。考虑了一些二维和三维几何特性。面积、周长和二维欧拉数是二维二值图像的性质。体积、表面积、平均宽度(也称为平均曲率积分)和三维欧拉数是三维二值图像的属性。孔隙率和物体数量也被认为是回归模型的参数。为了进行线性回归,对24个参数进行了评估,并选择了其中的一些参数。在大量研究的基础上,提出了预测岩石渗透率的方程。该方程有两组参数系数,一组预测高渗透岩石(大于2达西),另一组预测中、低渗透岩石(小于2达西),可用于碳酸盐岩。实验案例的平均绝对相对误差为0.06。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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