Multiscale Research on Pore Structure Characteristics and Permeability Prediction of Sandstone

The random existence of many irregular pore structures in geotechnical materials has a decisive influence on its permeability and other macroscopic properties. The analysis and characterization of the micropore structure of the material and its permeability are of great significance for geotechnical...

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Main Authors: M. A. Shi-Jia, L. I. N. Yuan-Jian, L. I. U. Jiang-Feng, Kundwa Marie Judith, Ishimwe Hubert, W. A. N. G. Pei-lin
Format: Article
Language:English
Published: Wiley 2021-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2021/3356645
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author M. A. Shi-Jia
L. I. N. Yuan-Jian
L. I. U. Jiang-Feng
Kundwa Marie Judith
Ishimwe Hubert
W. A. N. G. Pei-lin
author_facet M. A. Shi-Jia
L. I. N. Yuan-Jian
L. I. U. Jiang-Feng
Kundwa Marie Judith
Ishimwe Hubert
W. A. N. G. Pei-lin
author_sort M. A. Shi-Jia
collection DOAJ
description The random existence of many irregular pore structures in geotechnical materials has a decisive influence on its permeability and other macroscopic properties. The analysis and characterization of the micropore structure of the material and its permeability are of great significance for geotechnical engineering. In this study, digital images with different magnifications were used to examine the pore structure and permeability of sandstone samples. The image processing method is used to obtain binary images, and then, the pore size distribution method is used to calculate the pore size distribution. Therefore, based on the Hagen-Poiseuille formula, we get the prediction value of material’s permeability and compare it with the value obtained from mercury intrusion porosimetry (MIP). It is found that different microscopic images with different magnification and various statistical methods of pore size have a specific influence on the characterization of pore structure and permeability prediction. The porosity of different magnifications is not the same, and the results obtained at higher magnifications are more consistent with the results obtained with MIP. With the increase of magnification, we can observe more pores in large sizes. The effect of CPSD (continuous pore size distribution) in pore size statistics is better than that of DPSD (discrete pore size distribution). In permeability prediction, the prediction result of higher magnification images are closer to the instrument test value, and the value of DPSD is more significant than that of CPSD. In future research, an appropriate method should be selected to obtain a reasonable prediction of the permeability of the target material.
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spelling doaj-art-c424f9b42fdf46c798d0a4038544fa6f2025-08-20T02:18:55ZengWileyGeofluids1468-81232021-01-01202110.1155/2021/3356645Multiscale Research on Pore Structure Characteristics and Permeability Prediction of SandstoneM. A. Shi-Jia0L. I. N. Yuan-Jian1L. I. U. Jiang-Feng2Kundwa Marie Judith3Ishimwe Hubert4W. A. N. G. Pei-lin5The State Key Laboratory for GeoMechanics and Deep Underground EngineeringThe State Key Laboratory for GeoMechanics and Deep Underground EngineeringThe State Key Laboratory for GeoMechanics and Deep Underground EngineeringThe State Key Laboratory for GeoMechanics and Deep Underground EngineeringSchool of Resources and GeosciencesThe State Key Laboratory for GeoMechanics and Deep Underground EngineeringThe random existence of many irregular pore structures in geotechnical materials has a decisive influence on its permeability and other macroscopic properties. The analysis and characterization of the micropore structure of the material and its permeability are of great significance for geotechnical engineering. In this study, digital images with different magnifications were used to examine the pore structure and permeability of sandstone samples. The image processing method is used to obtain binary images, and then, the pore size distribution method is used to calculate the pore size distribution. Therefore, based on the Hagen-Poiseuille formula, we get the prediction value of material’s permeability and compare it with the value obtained from mercury intrusion porosimetry (MIP). It is found that different microscopic images with different magnification and various statistical methods of pore size have a specific influence on the characterization of pore structure and permeability prediction. The porosity of different magnifications is not the same, and the results obtained at higher magnifications are more consistent with the results obtained with MIP. With the increase of magnification, we can observe more pores in large sizes. The effect of CPSD (continuous pore size distribution) in pore size statistics is better than that of DPSD (discrete pore size distribution). In permeability prediction, the prediction result of higher magnification images are closer to the instrument test value, and the value of DPSD is more significant than that of CPSD. In future research, an appropriate method should be selected to obtain a reasonable prediction of the permeability of the target material.http://dx.doi.org/10.1155/2021/3356645
spellingShingle M. A. Shi-Jia
L. I. N. Yuan-Jian
L. I. U. Jiang-Feng
Kundwa Marie Judith
Ishimwe Hubert
W. A. N. G. Pei-lin
Multiscale Research on Pore Structure Characteristics and Permeability Prediction of Sandstone
Geofluids
title Multiscale Research on Pore Structure Characteristics and Permeability Prediction of Sandstone
title_full Multiscale Research on Pore Structure Characteristics and Permeability Prediction of Sandstone
title_fullStr Multiscale Research on Pore Structure Characteristics and Permeability Prediction of Sandstone
title_full_unstemmed Multiscale Research on Pore Structure Characteristics and Permeability Prediction of Sandstone
title_short Multiscale Research on Pore Structure Characteristics and Permeability Prediction of Sandstone
title_sort multiscale research on pore structure characteristics and permeability prediction of sandstone
url http://dx.doi.org/10.1155/2021/3356645
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