The Effect of Pre-heating Treatment and Water–Cement Ratio on the Shearing Behavior and Permeability of Granite–Cement Interface Samples

The shearing behavior and permeability of the interfaces between rock and cement are critical for the stability analysis of supporting structures in underground engineering projects, especially after exposure to thermal loads. In the present study, an advanced test method was proposed to preform she...

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Veröffentlicht in:Rock mechanics and rock engineering 2021-11, Vol.54 (11), p.5639-5650
Hauptverfasser: Zhang, Fan, Cheng, Tanzhuo, Zhu, Zhenzhen, Hu, Dawei, Shao, Jianfu
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container_issue 11
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creator Zhang, Fan
Cheng, Tanzhuo
Zhu, Zhenzhen
Hu, Dawei
Shao, Jianfu
description The shearing behavior and permeability of the interfaces between rock and cement are critical for the stability analysis of supporting structures in underground engineering projects, especially after exposure to thermal loads. In the present study, an advanced test method was proposed to preform shearing tests on granite–cement interface samples after pre-heating treatment. The samples consisted of two semi-cylindrical parts. The first part was granite, and the other was cement with two different water–cement ratios (for example, 0.3 and 0.5). The shear stress–strain curves, peak shear strength at shear failure, as well as the residual shear strength at the residual shear stage, cohesion, and internal shear angle, were analyzed. The results were correlated to the pre-heating temperatures and cement–water ratios, while the initial permeability before shear loading, along with the permeability evolution during the shearing process, was also analyzed. It was found that after higher pre-heating treatment the lower the peak shear strength, cohesion, and internal friction angle of the samples would be. Meanwhile, the initial permeability was higher. In addition, during the shearing process, the shear stress and permeability levels increased rapidly, reaching maximum values when shear failure occurred. Then, the shear stress and permeability levels decreased gradually to stable values at the residual shear stage. The degradation in the shear strength, cohesion, and internal friction angle caused by the pre-heating treatment may be attributed to the microcracks induced by the thermal expansion differences between the granite and cement and the evaporation of the chemically bound water in the cement. The shearing behavior and permeability evolution of the granite–cement interface samples were determined to be closely related to the water–cement ratios. For example, under the same normal stress and pre-heating temperature conditions, when the water–cement ratio was higher, the porosity of the cement was greater and the adhesion between the granite–cement interfaces was lower. Therefore, the peak shear strength at the shear failure point was also lower. In addition, the shear stress–strain curves showed stronger ductile behavior, and the cohesion and internal friction angle were lower. Meanwhile, the reductions in the shear stress and permeability levels at the residual shear stage became smaller.
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In addition, during the shearing process, the shear stress and permeability levels increased rapidly, reaching maximum values when shear failure occurred. Then, the shear stress and permeability levels decreased gradually to stable values at the residual shear stage. The degradation in the shear strength, cohesion, and internal friction angle caused by the pre-heating treatment may be attributed to the microcracks induced by the thermal expansion differences between the granite and cement and the evaporation of the chemically bound water in the cement. The shearing behavior and permeability evolution of the granite–cement interface samples were determined to be closely related to the water–cement ratios. For example, under the same normal stress and pre-heating temperature conditions, when the water–cement ratio was higher, the porosity of the cement was greater and the adhesion between the granite–cement interfaces was lower. 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In addition, during the shearing process, the shear stress and permeability levels increased rapidly, reaching maximum values when shear failure occurred. Then, the shear stress and permeability levels decreased gradually to stable values at the residual shear stage. The degradation in the shear strength, cohesion, and internal friction angle caused by the pre-heating treatment may be attributed to the microcracks induced by the thermal expansion differences between the granite and cement and the evaporation of the chemically bound water in the cement. The shearing behavior and permeability evolution of the granite–cement interface samples were determined to be closely related to the water–cement ratios. For example, under the same normal stress and pre-heating temperature conditions, when the water–cement ratio was higher, the porosity of the cement was greater and the adhesion between the granite–cement interfaces was lower. 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In the present study, an advanced test method was proposed to preform shearing tests on granite–cement interface samples after pre-heating treatment. The samples consisted of two semi-cylindrical parts. The first part was granite, and the other was cement with two different water–cement ratios (for example, 0.3 and 0.5). The shear stress–strain curves, peak shear strength at shear failure, as well as the residual shear strength at the residual shear stage, cohesion, and internal shear angle, were analyzed. The results were correlated to the pre-heating temperatures and cement–water ratios, while the initial permeability before shear loading, along with the permeability evolution during the shearing process, was also analyzed. It was found that after higher pre-heating treatment the lower the peak shear strength, cohesion, and internal friction angle of the samples would be. Meanwhile, the initial permeability was higher. In addition, during the shearing process, the shear stress and permeability levels increased rapidly, reaching maximum values when shear failure occurred. Then, the shear stress and permeability levels decreased gradually to stable values at the residual shear stage. The degradation in the shear strength, cohesion, and internal friction angle caused by the pre-heating treatment may be attributed to the microcracks induced by the thermal expansion differences between the granite and cement and the evaporation of the chemically bound water in the cement. The shearing behavior and permeability evolution of the granite–cement interface samples were determined to be closely related to the water–cement ratios. For example, under the same normal stress and pre-heating temperature conditions, when the water–cement ratio was higher, the porosity of the cement was greater and the adhesion between the granite–cement interfaces was lower. Therefore, the peak shear strength at the shear failure point was also lower. In addition, the shear stress–strain curves showed stronger ductile behavior, and the cohesion and internal friction angle were lower. Meanwhile, the reductions in the shear stress and permeability levels at the residual shear stage became smaller.</abstract><cop>Vienna</cop><pub>Springer Vienna</pub><doi>10.1007/s00603-021-02574-0</doi><tpages>12</tpages><orcidid>https://orcid.org/0000-0002-6632-8207</orcidid></addata></record>
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source Springer Nature - Complete Springer Journals
subjects Bound water
Cement
Civil Engineering
Cohesion
Concrete
Earth and Environmental Science
Earth Sciences
Engineering Sciences
Evaporation
Evolution
Failure
Friction
Geophysics/Geodesy
Granite
Heating
Interface stability
Interfaces
Internal friction
Mechanics
Microcracks
Original Paper
Permeability
Porosity
Ratios
Shear strength
Shear stress
Shearing
Stability
Stability analysis
Stress-strain curves
Stress-strain relations
Structural stability
Thermal analysis
Thermal expansion
Underground structures
Water
Water-cement ratio
title The Effect of Pre-heating Treatment and Water–Cement Ratio on the Shearing Behavior and Permeability of Granite–Cement Interface Samples
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