Permeability Evolution of an Intact Marble Core during Shearing under High Fluid Pressure

The progressive shear failure of a rock mass under hydromechanical coupling is a key aspect of the long-term stability of deeply buried, high fluid pressure diversion tunnels. In this study, we use experimental and numerical analysis to quantify the permeability variations that occur in an intact ma...

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Main Authors: Yuan Wang, Yu Jiao, Shaobin Hu
Format: Article
Language:English
Published: Wiley 2021-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2021/8870890
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author Yuan Wang
Yu Jiao
Shaobin Hu
author_facet Yuan Wang
Yu Jiao
Shaobin Hu
author_sort Yuan Wang
collection DOAJ
description The progressive shear failure of a rock mass under hydromechanical coupling is a key aspect of the long-term stability of deeply buried, high fluid pressure diversion tunnels. In this study, we use experimental and numerical analysis to quantify the permeability variations that occur in an intact marble sample as it evolves from shear failure to shear slip under different confining pressures and fluid pressures. The experimental results reveal that at low effective normal stress, the fracture permeability is positively correlated with the shear displacement. The permeability is lower at higher effective normal stress and exhibits an episodic change with increasing shear displacement. After establishing a numerical model based on the point cloud data generated by the three-dimensional (3D) laser scanning of the fracture surfaces, we found that there are some contact areas that block the percolation channels under high effective stress conditions. This type of contact area plays a key role in determining the evolution of the fracture permeability in a given rock sample.
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institution Kabale University
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publishDate 2021-01-01
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spelling doaj-art-8054dfed098b433bb5dc699e605bc9192025-02-03T01:28:18ZengWileyGeofluids1468-81151468-81232021-01-01202110.1155/2021/88708908870890Permeability Evolution of an Intact Marble Core during Shearing under High Fluid PressureYuan Wang0Yu Jiao1Shaobin Hu2College of Water Conservancy and Hydropower Engineering, Hohai University, Nanjing 210096, ChinaCollege of Civil and Transportation Engineering, Hohai University, Nanjing 210096, ChinaCollege of Civil and Transportation Engineering, Hohai University, Nanjing 210096, ChinaThe progressive shear failure of a rock mass under hydromechanical coupling is a key aspect of the long-term stability of deeply buried, high fluid pressure diversion tunnels. In this study, we use experimental and numerical analysis to quantify the permeability variations that occur in an intact marble sample as it evolves from shear failure to shear slip under different confining pressures and fluid pressures. The experimental results reveal that at low effective normal stress, the fracture permeability is positively correlated with the shear displacement. The permeability is lower at higher effective normal stress and exhibits an episodic change with increasing shear displacement. After establishing a numerical model based on the point cloud data generated by the three-dimensional (3D) laser scanning of the fracture surfaces, we found that there are some contact areas that block the percolation channels under high effective stress conditions. This type of contact area plays a key role in determining the evolution of the fracture permeability in a given rock sample.http://dx.doi.org/10.1155/2021/8870890
spellingShingle Yuan Wang
Yu Jiao
Shaobin Hu
Permeability Evolution of an Intact Marble Core during Shearing under High Fluid Pressure
Geofluids
title Permeability Evolution of an Intact Marble Core during Shearing under High Fluid Pressure
title_full Permeability Evolution of an Intact Marble Core during Shearing under High Fluid Pressure
title_fullStr Permeability Evolution of an Intact Marble Core during Shearing under High Fluid Pressure
title_full_unstemmed Permeability Evolution of an Intact Marble Core during Shearing under High Fluid Pressure
title_short Permeability Evolution of an Intact Marble Core during Shearing under High Fluid Pressure
title_sort permeability evolution of an intact marble core during shearing under high fluid pressure
url http://dx.doi.org/10.1155/2021/8870890
work_keys_str_mv AT yuanwang permeabilityevolutionofanintactmarblecoreduringshearingunderhighfluidpressure
AT yujiao permeabilityevolutionofanintactmarblecoreduringshearingunderhighfluidpressure
AT shaobinhu permeabilityevolutionofanintactmarblecoreduringshearingunderhighfluidpressure