Predicting elastic properties and permeability of rocks from 2D thin sections

被引:4
|
作者
Srisutthiyakorn N. [1 ]
Hunter S. [2 ]
Sarker R. [2 ]
Hofmann R. [2 ]
Espejo I. [2 ]
机构
[1] Stanford University, Stanford, CA
[2] Shell International EandP, Houston, TX
来源
Srisutthiyakorn, Nattavadee (natts@stanford.edu) | 2018年 / Society of Exploration Geophysicists卷 / 37期
关键词
2D; 3D; Bulk modulus; Rock physics; Shear modulus;
D O I
10.1190/tle37060421.1
中图分类号
学科分类号
摘要
Predicting rock elastic properties and permeability from high-resolution 2D thin sections has been a challenging problem in rock physics because the 2D thin sections reveal very little about how the microstructure connects in the third dimension. However, 2D thin sections are widely available and inexpensive because they are often produced as a part of the reservoir-quality workflow. Furthermore, they have much higher resolution and greater field of view than micro X-ray computed tomography images, which are commonly used for rock properties estimation. The 2D thin sections we studied are from various hydrocarbon-bearing clastic formations with a variety of provenances, depositional environments, and burial histories. The high-resolution 2D images were scanned from these physical 2D thin sections. K-means segmentation was then employed to identify different minerals and pores for creating 2D binary images. The focus of this study is to simulate 2D elastic properties and permeability from 2D thin sections and then to employ various empirical relations to transform these 2D simulation results to 3D intrinsic rock properties. We compared the rock properties from this process to those from core measurements and measured wireline logs and found that these 2D to 3D rock property transformations yield promising results, especially for elastic properties. The results show that 2D thin section images have high enough resolution to resolve grain contacts very well. Predicting the permeability from 2D thin sections is still challenging since the process requires fitting the physical equation in order to retrieve the fitting coefficient for prediction due to our lack of understanding of the difference between 2D and 3D pore size distribution. © 2018 © 2018 by The Society of Exploration Geophysicists.
引用
收藏
页码:421 / 427
页数:6
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