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Investigation of internal damage evolution in gneiss considering water softening

In soft rock tunnels, there are often large deformations during construction, especially when the groundwater seepage and softens the surrounding rock. For achieving the purpose of studying the softening effect of water immersion on strength and stability of surrounding rock, 15 rock samples were se...

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Autores principales: Sun, Changhai, Xie, Bingxin, Wang, Rui, Deng, Xianghui, Wu, Jin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10403494/
https://www.ncbi.nlm.nih.gov/pubmed/37542192
http://dx.doi.org/10.1038/s41598-023-39664-8
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author Sun, Changhai
Xie, Bingxin
Wang, Rui
Deng, Xianghui
Wu, Jin
author_facet Sun, Changhai
Xie, Bingxin
Wang, Rui
Deng, Xianghui
Wu, Jin
author_sort Sun, Changhai
collection PubMed
description In soft rock tunnels, there are often large deformations during construction, especially when the groundwater seepage and softens the surrounding rock. For achieving the purpose of studying the softening effect of water immersion on strength and stability of surrounding rock, 15 rock samples were selected for physical and mechanical tests under 5 conditions: natural state and free immersion for 1, 3, 6, and 9 months, and nuclear magnetic resonance technology(NMR) was also adopted to test the internal pore structure of specimens with different immersion durations, thus the micro structure features of the gneiss, such as the NMR relaxation time T2 spectrum distribution, porosity, and pore volume ratio of different pore sizes under water softening were then obtained. The NMR results shows that the longer the free immersion duration of the rock sample, the greater the porosity; at the same time, the number of micropores in the rock gradually decreases under the interaction of water and rock, and the mesopores increase slightly first and then decrease all the time. The number of macropores is gradually increasing. When the immersion duration is 6 months, the number of macropores begins to increase significantly, and the mechanical properties of the specimens begin to drop significantly. By 9 months, the proportion of macropores in the rock has reached 57.6%. The results showed that the number growth of macropores is the root cause of the macroscopic failure of rock sample. The study results have significance for on-site construction in water-rich areas.
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spelling pubmed-104034942023-08-06 Investigation of internal damage evolution in gneiss considering water softening Sun, Changhai Xie, Bingxin Wang, Rui Deng, Xianghui Wu, Jin Sci Rep Article In soft rock tunnels, there are often large deformations during construction, especially when the groundwater seepage and softens the surrounding rock. For achieving the purpose of studying the softening effect of water immersion on strength and stability of surrounding rock, 15 rock samples were selected for physical and mechanical tests under 5 conditions: natural state and free immersion for 1, 3, 6, and 9 months, and nuclear magnetic resonance technology(NMR) was also adopted to test the internal pore structure of specimens with different immersion durations, thus the micro structure features of the gneiss, such as the NMR relaxation time T2 spectrum distribution, porosity, and pore volume ratio of different pore sizes under water softening were then obtained. The NMR results shows that the longer the free immersion duration of the rock sample, the greater the porosity; at the same time, the number of micropores in the rock gradually decreases under the interaction of water and rock, and the mesopores increase slightly first and then decrease all the time. The number of macropores is gradually increasing. When the immersion duration is 6 months, the number of macropores begins to increase significantly, and the mechanical properties of the specimens begin to drop significantly. By 9 months, the proportion of macropores in the rock has reached 57.6%. The results showed that the number growth of macropores is the root cause of the macroscopic failure of rock sample. The study results have significance for on-site construction in water-rich areas. Nature Publishing Group UK 2023-08-04 /pmc/articles/PMC10403494/ /pubmed/37542192 http://dx.doi.org/10.1038/s41598-023-39664-8 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
Sun, Changhai
Xie, Bingxin
Wang, Rui
Deng, Xianghui
Wu, Jin
Investigation of internal damage evolution in gneiss considering water softening
title Investigation of internal damage evolution in gneiss considering water softening
title_full Investigation of internal damage evolution in gneiss considering water softening
title_fullStr Investigation of internal damage evolution in gneiss considering water softening
title_full_unstemmed Investigation of internal damage evolution in gneiss considering water softening
title_short Investigation of internal damage evolution in gneiss considering water softening
title_sort investigation of internal damage evolution in gneiss considering water softening
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10403494/
https://www.ncbi.nlm.nih.gov/pubmed/37542192
http://dx.doi.org/10.1038/s41598-023-39664-8
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