Study on the cyclic shear mechanical properties of anchoring systems containing anchor cable,anchoring agent and surrounding rock

The interfaces between the anchor cable,anchoring agent and surrounding rock represent critical weak points in anchoring systems. This study focuses on the debonding failure characteristics under cyclic disturbance and established an equivalent shear mechanics model for the anchoring system,conducting cyclic shear tests. The influences of rock lithology,normal load(<italic>F</italic><sub>s</sub>),cyclic shear displacement amplitude(<italic>u</italic><sub>d</sub>) and cycle number(<italic>N</italic>) on the shear mechanical properties of the anchoring system were investigated. The experimental results reveal that the anchoring system experiences progressive accumulation of damage during the cyclic shear stage,with the maximum shear force(<italic>F</italic><sub>hpeak</sub>) generally presenting a decreasing trend as <italic>N</italic> increases. As <italic>u</italic><sub>d</sub> increases,the location of the maximum shear force in the anchoring system gradually shifts from the direct shear stage to the cyclic shear stage. The peak shear force(<italic>F</italic><sub>hmax</sub>) and residual shear force(<italic>F</italic><sub>hres</sub>) decrease by 28.46%–54.13% and 21.22%–49.25%,respectively. An increase in the rock strength and normal load enhances the shear resistance characteristics of the anchoring system. During the cyclic shear stage,the sustained wear and degradation at the interface result in a more pronounced normal shear contraction within the anchoring system. Conversely,in the direct shear process,the climbing effect of the through fracture plane leads to a gradual increase in normal shear dilation. The overall shear contraction of the anchoring system is gradually enhanced with increases in <italic>u</italic><sub>d</sub> and <italic>F</italic><sub>s</sub>,while it diminishes with increasing rock strength. Three typical shear failure modes of the anchoring system are identified:internal shear fracture through the coal matrix,debonding failure and fracture at the anchoring agent-sandstone interface,and debonding and slip at the anchor cable-anchoring agent interface in the limestone anchoring system. The entire process of shear fracture surface formation and the evolution of debonding failure in the anchoring system is discussed based on digital photography.

Authors

Publication Details

Journal
Chinese Journal of Rock Mechanics and Engineering
Published
2025-05-01
DOI
https://doi.org/10.3724/1000-6915.jrme.2024.0756
Citations
1
Primary Topic
Geotechnical and Geomechanical Engineering
Type
article
Field-Weighted Citation Impact
0.86
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article

Study on the cyclic shear mechanical properties of anchoring systems containing anchor cable,anchoring agent and surrounding rock

Manchao He, Qiang Zhu, Shi-Jun Ren, Jiangyu Wu et al.
1 citations
Chinese Journal of Rock Mechanics and Engineering
Geotechnical and Geomechanical Engineering
0.86
article

Study on the cyclic shear mechanical properties of anchoring systems containing anchor cable,anchoring agent and surrounding rock

Manchao He, Qiang Zhu, Shi-Jun Ren, Jiangyu Wu, Zhigang Tao, Hai Pu, F Wang, Yin Qian, Zhan Lyu
article en
1 citations

Abstract

The interfaces between the anchor cable,anchoring agent and surrounding rock represent critical weak points in anchoring systems. This study focuses on the debonding failure characteristics under cyclic disturbance and established an equivalent shear mechanics model for the anchoring system,conducting cyclic shear tests. The influences of rock lithology,normal load(<italic>F</italic><sub>s</sub>),cyclic shear displacement amplitude(<italic>u</italic><sub>d</sub>) and cycle number(<italic>N</italic>) on the shear mechanical properties of the anchoring system were investigated. The experimental results reveal that the anchoring system experiences progressive accumulation of damage during the cyclic shear stage,with the maximum shear force(<italic>F</italic><sub>hpeak</sub>) generally presenting a decreasing trend as <italic>N</italic> increases. As <italic>u</italic><sub>d</sub> increases,the location of the maximum shear force in the anchoring system gradually shifts from the direct shear stage to the cyclic shear stage. The peak shear force(<italic>F</italic><sub>hmax</sub>) and residual shear force(<italic>F</italic><sub>hres</sub>) decrease by 28.46%–54.13% and 21.22%–49.25%,respectively. An increase in the rock strength and normal load enhances the shear resistance characteristics of the anchoring system. During the cyclic shear stage,the sustained wear and degradation at the interface result in a more pronounced normal shear contraction within the anchoring system. Conversely,in the direct shear process,the climbing effect of the through fracture plane leads to a gradual increase in normal shear dilation. The overall shear contraction of the anchoring system is gradually enhanced with increases in <italic>u</italic><sub>d</sub> and <italic>F</italic><sub>s</sub>,while it diminishes with increasing rock strength. Three typical shear failure modes of the anchoring system are identified:internal shear fracture through the coal matrix,debonding failure and fracture at the anchoring agent-sandstone interface,and debonding and slip at the anchor cable-anchoring agent interface in the limestone anchoring system. The entire process of shear fracture surface formation and the evolution of debonding failure in the anchoring system is discussed based on digital photography.

Chinese Journal of Rock Mechanics and EngineeringVol. 44(5)
Openalex Percentile: Top 29%
Geotechnical and Geomechanical Engineering
0.86
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