Permeability Evolution and Particle Size Distribution of Saturated Crushed Sandstone under Compression

In this research, the particle size distribution and permeability of saturated crushed sandstone under variable axial stresses (0, 2, 4, 8, 12, and 16 MPa) were studied. X-ray Computed Tomography results revealed that particle crushing is likely to occur considerably as the axial stress is approachi...

Full description

Bibliographic Details
Main Authors: Chen, Y., Yu, B., Zhang, K., Zhang, M., Xu, Guang, Chen, Z.
Format: Journal Article
Published: Blackwell Publishing 2018
Online Access:http://hdl.handle.net/20.500.11937/60774
_version_ 1848760633695141888
author Chen, Y.
Yu, B.
Zhang, K.
Zhang, M.
Xu, Guang
Chen, Z.
author_facet Chen, Y.
Yu, B.
Zhang, K.
Zhang, M.
Xu, Guang
Chen, Z.
author_sort Chen, Y.
building Curtin Institutional Repository
collection Online Access
description In this research, the particle size distribution and permeability of saturated crushed sandstone under variable axial stresses (0, 2, 4, 8, 12, and 16 MPa) were studied. X-ray Computed Tomography results revealed that particle crushing is likely to occur considerably as the axial stress is approaching 4 MPa, which results in the change of pore structure greatly. During compression, the particle size distribution satisfies the fractal condition well, and the fractal dimension of particle size distribution is an effective method for describing the particle crushing state of saturated crushed sandstone. When the axial stress increases from 0 MPa to 4 MPa, the fractal dimension of the particle size distribution increases rapidly by over 60% of the total increase (0–16 MPa), and the permeability decreases sharply by about 85% of the total decrease. These results indicate that 4 MPa is a key value in controlling the particle size distribution and the permeability of the saturated crushed sandstone under axial compression. The permeability is influenced by the initial gradation of the specimens, and a larger Talbot exponent corresponds to a larger permeability.
first_indexed 2025-11-14T10:18:53Z
format Journal Article
id curtin-20.500.11937-60774
institution Curtin University Malaysia
institution_category Local University
last_indexed 2025-11-14T10:18:53Z
publishDate 2018
publisher Blackwell Publishing
recordtype eprints
repository_type Digital Repository
spelling curtin-20.500.11937-607742018-06-29T02:03:47Z Permeability Evolution and Particle Size Distribution of Saturated Crushed Sandstone under Compression Chen, Y. Yu, B. Zhang, K. Zhang, M. Xu, Guang Chen, Z. In this research, the particle size distribution and permeability of saturated crushed sandstone under variable axial stresses (0, 2, 4, 8, 12, and 16 MPa) were studied. X-ray Computed Tomography results revealed that particle crushing is likely to occur considerably as the axial stress is approaching 4 MPa, which results in the change of pore structure greatly. During compression, the particle size distribution satisfies the fractal condition well, and the fractal dimension of particle size distribution is an effective method for describing the particle crushing state of saturated crushed sandstone. When the axial stress increases from 0 MPa to 4 MPa, the fractal dimension of the particle size distribution increases rapidly by over 60% of the total increase (0–16 MPa), and the permeability decreases sharply by about 85% of the total decrease. These results indicate that 4 MPa is a key value in controlling the particle size distribution and the permeability of the saturated crushed sandstone under axial compression. The permeability is influenced by the initial gradation of the specimens, and a larger Talbot exponent corresponds to a larger permeability. 2018 Journal Article http://hdl.handle.net/20.500.11937/60774 10.1155/2018/6043420 http://creativecommons.org/licenses/by/4.0/ Blackwell Publishing fulltext
spellingShingle Chen, Y.
Yu, B.
Zhang, K.
Zhang, M.
Xu, Guang
Chen, Z.
Permeability Evolution and Particle Size Distribution of Saturated Crushed Sandstone under Compression
title Permeability Evolution and Particle Size Distribution of Saturated Crushed Sandstone under Compression
title_full Permeability Evolution and Particle Size Distribution of Saturated Crushed Sandstone under Compression
title_fullStr Permeability Evolution and Particle Size Distribution of Saturated Crushed Sandstone under Compression
title_full_unstemmed Permeability Evolution and Particle Size Distribution of Saturated Crushed Sandstone under Compression
title_short Permeability Evolution and Particle Size Distribution of Saturated Crushed Sandstone under Compression
title_sort permeability evolution and particle size distribution of saturated crushed sandstone under compression
url http://hdl.handle.net/20.500.11937/60774