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Numerical simulation of size effect of defective rock under compression condition
The existence of various types of damage, small cracks, some large voids and the size of the sample in the rock will make the experimental results show great discreteness. In this paper, based on the results of laboratory experiments, a numerical model of large flawed rock samples is established by...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2023
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9829666/ https://www.ncbi.nlm.nih.gov/pubmed/36624260 http://dx.doi.org/10.1038/s41598-023-27651-y |
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author | Hu, Zeyu Xie, Liangfu Qin, Yongjun Liu, Xuejun Qian, Jiangu |
author_facet | Hu, Zeyu Xie, Liangfu Qin, Yongjun Liu, Xuejun Qian, Jiangu |
author_sort | Hu, Zeyu |
collection | PubMed |
description | The existence of various types of damage, small cracks, some large voids and the size of the sample in the rock will make the experimental results show great discreteness. In this paper, based on the results of laboratory experiments, a numerical model of large flawed rock samples is established by using particle flow software PFC2D, and the mechanical response of rocks with different length-diameter ratios and different flaw positions in uniaxial compression experiments is discussed. The results show that the specimen size has a significant effect on the crack characteristics, mechanical characteristics and energy characteristics of rock mass. From the perspective of energy and crack characteristics, the total number of cracks after the failure of the defective rock sample is slightly lower than that of the intact rock sample, resulting in a slightly lower peak strain energy during the rock failure process. From the mechanical properties of rock samples, the Poisson’s ratio of intact rock samples is slightly smaller than that of defective rock samples. The strength of the defective sample is weakened relative to the complete rock sample, and the relationship formula between the weakening range and the aspect ratio is obtained through analysis. Moreover, different defect locations lead to different crack processes and crack modes, resulting in different uniaxial compressive strength. |
format | Online Article Text |
id | pubmed-9829666 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2023 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-98296662023-01-11 Numerical simulation of size effect of defective rock under compression condition Hu, Zeyu Xie, Liangfu Qin, Yongjun Liu, Xuejun Qian, Jiangu Sci Rep Article The existence of various types of damage, small cracks, some large voids and the size of the sample in the rock will make the experimental results show great discreteness. In this paper, based on the results of laboratory experiments, a numerical model of large flawed rock samples is established by using particle flow software PFC2D, and the mechanical response of rocks with different length-diameter ratios and different flaw positions in uniaxial compression experiments is discussed. The results show that the specimen size has a significant effect on the crack characteristics, mechanical characteristics and energy characteristics of rock mass. From the perspective of energy and crack characteristics, the total number of cracks after the failure of the defective rock sample is slightly lower than that of the intact rock sample, resulting in a slightly lower peak strain energy during the rock failure process. From the mechanical properties of rock samples, the Poisson’s ratio of intact rock samples is slightly smaller than that of defective rock samples. The strength of the defective sample is weakened relative to the complete rock sample, and the relationship formula between the weakening range and the aspect ratio is obtained through analysis. Moreover, different defect locations lead to different crack processes and crack modes, resulting in different uniaxial compressive strength. Nature Publishing Group UK 2023-01-09 /pmc/articles/PMC9829666/ /pubmed/36624260 http://dx.doi.org/10.1038/s41598-023-27651-y Text en © The Author(s) 2023 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Article Hu, Zeyu Xie, Liangfu Qin, Yongjun Liu, Xuejun Qian, Jiangu Numerical simulation of size effect of defective rock under compression condition |
title | Numerical simulation of size effect of defective rock under compression condition |
title_full | Numerical simulation of size effect of defective rock under compression condition |
title_fullStr | Numerical simulation of size effect of defective rock under compression condition |
title_full_unstemmed | Numerical simulation of size effect of defective rock under compression condition |
title_short | Numerical simulation of size effect of defective rock under compression condition |
title_sort | numerical simulation of size effect of defective rock under compression condition |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9829666/ https://www.ncbi.nlm.nih.gov/pubmed/36624260 http://dx.doi.org/10.1038/s41598-023-27651-y |
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