Mechanical properties and dynamic breaking mechanism of plateau frozen soil

AbstractThis work studies and evaluates the mechanical properties of frozen soil, FS, from Yulong mine in Tibet, under different freezing temperatures ranging from −12 °C to −1 °C, using experimental tests. In addition, the effects of temperature and time on the freezing depth of FS were investigate...

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Published in:Geomatics, Natural Hazards and Risk
Main Authors: Fuqiang Ren, Changhao Hao, Bo Sun, Zhenyang Xu
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2023
Subjects:
geo
Online Access:https://doi.org/10.1080/19475705.2022.2164225
https://doaj.org/article/73fb2b07132c45f5b529c7b35a779fe0
id fttriple:oai:gotriple.eu:oai:doaj.org/article:73fb2b07132c45f5b529c7b35a779fe0
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:73fb2b07132c45f5b529c7b35a779fe0 2023-05-15T17:57:52+02:00 Mechanical properties and dynamic breaking mechanism of plateau frozen soil Fuqiang Ren Changhao Hao Bo Sun Zhenyang Xu 2023-12-01 https://doi.org/10.1080/19475705.2022.2164225 https://doaj.org/article/73fb2b07132c45f5b529c7b35a779fe0 en eng Taylor & Francis Group doi:10.1080/19475705.2022.2164225 1947-5713 1947-5705 https://doaj.org/article/73fb2b07132c45f5b529c7b35a779fe0 undefined Geomatics, Natural Hazards & Risk, Vol 14, Iss 1 (2023) Plateau permafrost freezing temperature mechanical properties breaking mechanism mechanical model envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2023 fttriple https://doi.org/10.1080/19475705.2022.2164225 2023-01-22T19:15:51Z AbstractThis work studies and evaluates the mechanical properties of frozen soil, FS, from Yulong mine in Tibet, under different freezing temperatures ranging from −12 °C to −1 °C, using experimental tests. In addition, the effects of temperature and time on the freezing depth of FS were investigated. Based on the cantilever beam theory, the mechanical model of FS breaking under blasting stress wave was established, and the theoretical formula for the fracture length (FL) of FS was deduced. Moreover, the major influences on FL were analyzed. The results showed that the frozen depth curves at different temperatures were approximately linear in single or double segments, and the lower the temperature, the greater the early freezing rate. Additionally, the uniaxial compression strength, elastic modulus, and tensile strength of FS were found to decrease with the increase in temperature. The findings highlight that the shear strength, cohesion, and internal friction angle decreased first and then increased with the increase in temperature. It was shown that the thickness, friction coefficient, weight density, and tensile strength of FS are positively correlated with the FL, while there is an inverse proportionality with respect to the pressure of the detonation wave. Article in Journal/Newspaper permafrost Unknown Geomatics, Natural Hazards and Risk 14 1
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic Plateau permafrost
freezing temperature
mechanical properties
breaking mechanism
mechanical model
envir
geo
spellingShingle Plateau permafrost
freezing temperature
mechanical properties
breaking mechanism
mechanical model
envir
geo
Fuqiang Ren
Changhao Hao
Bo Sun
Zhenyang Xu
Mechanical properties and dynamic breaking mechanism of plateau frozen soil
topic_facet Plateau permafrost
freezing temperature
mechanical properties
breaking mechanism
mechanical model
envir
geo
description AbstractThis work studies and evaluates the mechanical properties of frozen soil, FS, from Yulong mine in Tibet, under different freezing temperatures ranging from −12 °C to −1 °C, using experimental tests. In addition, the effects of temperature and time on the freezing depth of FS were investigated. Based on the cantilever beam theory, the mechanical model of FS breaking under blasting stress wave was established, and the theoretical formula for the fracture length (FL) of FS was deduced. Moreover, the major influences on FL were analyzed. The results showed that the frozen depth curves at different temperatures were approximately linear in single or double segments, and the lower the temperature, the greater the early freezing rate. Additionally, the uniaxial compression strength, elastic modulus, and tensile strength of FS were found to decrease with the increase in temperature. The findings highlight that the shear strength, cohesion, and internal friction angle decreased first and then increased with the increase in temperature. It was shown that the thickness, friction coefficient, weight density, and tensile strength of FS are positively correlated with the FL, while there is an inverse proportionality with respect to the pressure of the detonation wave.
format Article in Journal/Newspaper
author Fuqiang Ren
Changhao Hao
Bo Sun
Zhenyang Xu
author_facet Fuqiang Ren
Changhao Hao
Bo Sun
Zhenyang Xu
author_sort Fuqiang Ren
title Mechanical properties and dynamic breaking mechanism of plateau frozen soil
title_short Mechanical properties and dynamic breaking mechanism of plateau frozen soil
title_full Mechanical properties and dynamic breaking mechanism of plateau frozen soil
title_fullStr Mechanical properties and dynamic breaking mechanism of plateau frozen soil
title_full_unstemmed Mechanical properties and dynamic breaking mechanism of plateau frozen soil
title_sort mechanical properties and dynamic breaking mechanism of plateau frozen soil
publisher Taylor & Francis Group
publishDate 2023
url https://doi.org/10.1080/19475705.2022.2164225
https://doaj.org/article/73fb2b07132c45f5b529c7b35a779fe0
genre permafrost
genre_facet permafrost
op_source Geomatics, Natural Hazards & Risk, Vol 14, Iss 1 (2023)
op_relation doi:10.1080/19475705.2022.2164225
1947-5713
1947-5705
https://doaj.org/article/73fb2b07132c45f5b529c7b35a779fe0
op_rights undefined
op_doi https://doi.org/10.1080/19475705.2022.2164225
container_title Geomatics, Natural Hazards and Risk
container_volume 14
container_issue 1
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