Machine Learning for 3D Image Recognition to Determine Porosity and Lithology of Heterogeneous Carbonate Rock

Omar Al-Farisi, Hongtao Zhang, Aikifa Raza, Djamel Ozzane, M. Sassi, TieJun Zhang
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引用次数: 7

Abstract

Automated image processing algorithms can improve the quality and speed of classifying the morphology of heterogeneous carbonate rock. Several commercial products have worked to produce petrophysical properties from 2D images and with less extent from 3D images, relying on image processing and flow simulation. Images are mainly micro-computed tomography (μCT), optical images of thin-section, or magnetic resonance images (MRI). However, most of the successful work is from the homogeneous and clastic rocks. In this work, we have demonstrated a Machine Learning assisted Image Recognition (MLIR) approach to determine the porosity and lithology of heterogeneous carbonate rock by analyzing 3D images form μCT and MRI. Our research method consists of two parts: experimental and MLIR. Experimentally, we measured porosity of rock core plug with three different ways: (i) weight difference of dry and saturated rock, (ii) NMR T2 relaxation of saturated rock, and (iii) helium gas injection of rock after cleaning and drying. We performed MLIR on 3D μCT and MRI images using random forest machine-learning algorithm. Petrophysicist provided a set of training data with classes (i.e., limestone, pyrite, and pore) as expert knowledge of μCT Image intensity correspondence to petrophysical properties. MLIR performed, alone, each task for identifying different lithology types and porosity. Determined volumes have been checked and confirmed with three different experimental datasets. The measured porosity, from three experiment-based approaches, is very close. Similarly, the MLR measured porosity produced excellent results comparatively with three experimental measurements, with an accuracy of 97.1% on the training set and 94.4% on blind test prediction.
基于机器学习的三维图像识别方法确定非均质碳酸盐岩孔隙度和岩性
自动图像处理算法可以提高非均质碳酸盐岩形态分类的质量和速度。一些商业产品依靠图像处理和流动模拟,从2D图像和较少程度的3D图像中获得岩石物理性质。图像主要是微计算机断层扫描(μCT)、薄层光学图像或磁共振图像(MRI)。然而,大多数成功的工作是来自均质岩和碎屑岩。在这项工作中,我们展示了一种机器学习辅助图像识别(MLIR)方法,通过分析μCT和MRI的3D图像来确定非均质碳酸盐岩的孔隙度和岩性。我们的研究方法包括两个部分:实验和MLIR。实验中,我们采用三种不同的方法测量岩心塞的孔隙度:(i)干燥岩石的质量差,(ii)饱和岩石的核磁共振T2弛豫,(iii)岩石清洗干燥后的氦气注入。我们使用随机森林机器学习算法对三维μCT和MRI图像进行MLIR。岩石物理学家提供了一组带有类(石灰石、黄铁矿、孔隙)的训练数据,作为μCT图像强度与岩石物性对应的专家知识。MLIR单独完成了识别不同岩性和孔隙度的每项任务。已确定的体积用三个不同的实验数据集进行了检查和确认。通过三种基于实验的方法测量的孔隙度非常接近。同样,MLR测量的孔隙度与三个实验测量结果相比也取得了很好的结果,在训练集上的准确率为97.1%,在盲测预测上的准确率为94.4%。
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