The Bolt Anchorage Performance of Fractured Rock under a Freeze–Thaw Cycle Load
In circumstances influenced by freeze–thaw cycles, the strength of rock diminishes, necessitating an in-depth investigation into its corresponding anchoring support schemes. This study conducted experiments on rocks with and without fractures at angles of 0°, 45°, and 90° subjected to freeze–thaw cy...
| Published in: | Applied Sciences |
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| Main Authors: | , |
| Format: | Article |
| Language: | English |
| Published: |
MDPI AG
2024-05-01
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| Online Access: | https://www.mdpi.com/2076-3417/14/10/4152 |
| _version_ | 1850358249431236608 |
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| author | Fengyan Han Yu Chen |
| author_facet | Fengyan Han Yu Chen |
| author_sort | Fengyan Han |
| collection | DOAJ |
| container_title | Applied Sciences |
| description | In circumstances influenced by freeze–thaw cycles, the strength of rock diminishes, necessitating an in-depth investigation into its corresponding anchoring support schemes. This study conducted experiments on rocks with and without fractures at angles of 0°, 45°, and 90° subjected to freeze–thaw cycles of 0, 10, 20, and 30 iterations. It explored the effects of fracture inclination, anchoring conditions, and freeze–thaw cycles on the mechanical properties of rock. The primary findings from the experiments are as follows: (1) fracture inclination significantly impacts rock strength, with the most pronounced deterioration observed in samples with a 45° fracture, exhibiting strengths and elastic moduli at 28.4% and 73.4%, respectively, of those of fracture-free samples; (2) anchoring effectively controls deformation but concurrently induces stress concentrations, resulting in Y-shaped crack formation around the anchoring rod; (3) the degree of strength reduction due to freeze–thaw cycles is angle-dependent, with fracture-free and 90° fracture samples exhibiting diminished strength post freezing, while the 45° fracture samples’ strength remains largely unchanged. Additionally, this study employed a numerical model, coupling a discrete element method (DEM) with a finite difference method (FDM), to simulate experimental conditions, yielding conclusions consistent with experimental outcomes, and notably revealing a prevalence of tensile cracks over shear cracks within samples under uniaxial compression. |
| format | Article |
| id | doaj-art-cbd70f033bc4445c8a7909bef931d85d |
| institution | Directory of Open Access Journals |
| issn | 2076-3417 |
| language | English |
| publishDate | 2024-05-01 |
| publisher | MDPI AG |
| record_format | Article |
| spelling | doaj-art-cbd70f033bc4445c8a7909bef931d85d2025-08-19T23:06:40ZengMDPI AGApplied Sciences2076-34172024-05-011410415210.3390/app14104152The Bolt Anchorage Performance of Fractured Rock under a Freeze–Thaw Cycle LoadFengyan Han0Yu Chen1School of Civil Engineering, Central South University, Changsha 410075, ChinaSchool of Civil Engineering, Sun Yat-sen University & Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519000, ChinaIn circumstances influenced by freeze–thaw cycles, the strength of rock diminishes, necessitating an in-depth investigation into its corresponding anchoring support schemes. This study conducted experiments on rocks with and without fractures at angles of 0°, 45°, and 90° subjected to freeze–thaw cycles of 0, 10, 20, and 30 iterations. It explored the effects of fracture inclination, anchoring conditions, and freeze–thaw cycles on the mechanical properties of rock. The primary findings from the experiments are as follows: (1) fracture inclination significantly impacts rock strength, with the most pronounced deterioration observed in samples with a 45° fracture, exhibiting strengths and elastic moduli at 28.4% and 73.4%, respectively, of those of fracture-free samples; (2) anchoring effectively controls deformation but concurrently induces stress concentrations, resulting in Y-shaped crack formation around the anchoring rod; (3) the degree of strength reduction due to freeze–thaw cycles is angle-dependent, with fracture-free and 90° fracture samples exhibiting diminished strength post freezing, while the 45° fracture samples’ strength remains largely unchanged. Additionally, this study employed a numerical model, coupling a discrete element method (DEM) with a finite difference method (FDM), to simulate experimental conditions, yielding conclusions consistent with experimental outcomes, and notably revealing a prevalence of tensile cracks over shear cracks within samples under uniaxial compression.https://www.mdpi.com/2076-3417/14/10/4152freeze–thaw cyclesfractured rockrock bolt |
| spellingShingle | Fengyan Han Yu Chen The Bolt Anchorage Performance of Fractured Rock under a Freeze–Thaw Cycle Load freeze–thaw cycles fractured rock rock bolt |
| title | The Bolt Anchorage Performance of Fractured Rock under a Freeze–Thaw Cycle Load |
| title_full | The Bolt Anchorage Performance of Fractured Rock under a Freeze–Thaw Cycle Load |
| title_fullStr | The Bolt Anchorage Performance of Fractured Rock under a Freeze–Thaw Cycle Load |
| title_full_unstemmed | The Bolt Anchorage Performance of Fractured Rock under a Freeze–Thaw Cycle Load |
| title_short | The Bolt Anchorage Performance of Fractured Rock under a Freeze–Thaw Cycle Load |
| title_sort | bolt anchorage performance of fractured rock under a freeze thaw cycle load |
| topic | freeze–thaw cycles fractured rock rock bolt |
| url | https://www.mdpi.com/2076-3417/14/10/4152 |
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