Evolution of cracks in the shear bands of granite residual soil

The evolution of shear bands and cracks plays an important role in landslides. However, there is no systematic method for classification of the cracks, which can be used to analyze the evolution of cracks in shear bands. In this study, X-ray computed tomography (CT) is used to observe the behavior o...

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Main Authors: Chengsheng Li, Lingwei Kong, Ran An
Format: Article
Language:English
Published: Elsevier 2022-12-01
Series:Journal of Rock Mechanics and Geotechnical Engineering
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S167477552200097X
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author Chengsheng Li
Lingwei Kong
Ran An
author_facet Chengsheng Li
Lingwei Kong
Ran An
author_sort Chengsheng Li
collection DOAJ
description The evolution of shear bands and cracks plays an important role in landslides. However, there is no systematic method for classification of the cracks, which can be used to analyze the evolution of cracks in shear bands. In this study, X-ray computed tomography (CT) is used to observe the behavior of granite residual soil during a triaxial shear process. Based on the digital volume correlation (DVC) method, a crack classification method is established according to the connectivity characteristics of cracks before and after loading. Cracks are then divided into six classes: obsolete, brand-new, isolated, split, combined, and compound. With evolution of the shear bands, a large number of brand-new cracks accelerate the damages of materials at the mesoscale, resulting in a sharp decrease in strength. The volume of brand-new cracks increases rapidly with increasing axial strain, and their volume is greater than 50% when the strain reaches 12%, while the volume of compound cracks decreases from 54% to 21%. As cracks are the weakest areas in a material, brand-new cracks accelerate the development of shear bands. Finally, the coupling effect of shear bands and cracks destroys the soil strength.
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spelling doaj.art-cb9692e9015d4b108d68d5a841a29cc72022-12-22T04:36:21ZengElsevierJournal of Rock Mechanics and Geotechnical Engineering1674-77552022-12-0114619561966Evolution of cracks in the shear bands of granite residual soilChengsheng Li0Lingwei Kong1Ran An2Department of Civil and Environmental Engineering, Shantou University, Shantou, 515063, China; State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, 430071, China; Corresponding author. Department of Civil and Environmental Engineering, Shantou University, Shantou, 515063, China.State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, 430071, ChinaState Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, 430071, China; College of Urban Construction, Wuhan University of Science and Technology, Wuhan, 430065, ChinaThe evolution of shear bands and cracks plays an important role in landslides. However, there is no systematic method for classification of the cracks, which can be used to analyze the evolution of cracks in shear bands. In this study, X-ray computed tomography (CT) is used to observe the behavior of granite residual soil during a triaxial shear process. Based on the digital volume correlation (DVC) method, a crack classification method is established according to the connectivity characteristics of cracks before and after loading. Cracks are then divided into six classes: obsolete, brand-new, isolated, split, combined, and compound. With evolution of the shear bands, a large number of brand-new cracks accelerate the damages of materials at the mesoscale, resulting in a sharp decrease in strength. The volume of brand-new cracks increases rapidly with increasing axial strain, and their volume is greater than 50% when the strain reaches 12%, while the volume of compound cracks decreases from 54% to 21%. As cracks are the weakest areas in a material, brand-new cracks accelerate the development of shear bands. Finally, the coupling effect of shear bands and cracks destroys the soil strength.http://www.sciencedirect.com/science/article/pii/S167477552200097XShear bandCrack classification methodDigital volume correlation (DVC)X-ray computed tomography (CT)Granite residual soil
spellingShingle Chengsheng Li
Lingwei Kong
Ran An
Evolution of cracks in the shear bands of granite residual soil
Journal of Rock Mechanics and Geotechnical Engineering
Shear band
Crack classification method
Digital volume correlation (DVC)
X-ray computed tomography (CT)
Granite residual soil
title Evolution of cracks in the shear bands of granite residual soil
title_full Evolution of cracks in the shear bands of granite residual soil
title_fullStr Evolution of cracks in the shear bands of granite residual soil
title_full_unstemmed Evolution of cracks in the shear bands of granite residual soil
title_short Evolution of cracks in the shear bands of granite residual soil
title_sort evolution of cracks in the shear bands of granite residual soil
topic Shear band
Crack classification method
Digital volume correlation (DVC)
X-ray computed tomography (CT)
Granite residual soil
url http://www.sciencedirect.com/science/article/pii/S167477552200097X
work_keys_str_mv AT chengshengli evolutionofcracksintheshearbandsofgraniteresidualsoil
AT lingweikong evolutionofcracksintheshearbandsofgraniteresidualsoil
AT ranan evolutionofcracksintheshearbandsofgraniteresidualsoil