REVIEW ON THE MECHANICAL PROPERTIES OF FROZEN ROCKS

The freezing technique has been employed for a long time to strengthen the mechanical properties of intact rock and rock mass; however, it has not received as much attention as it deserves. This paper thoroughly reviews the effect of freezing on the essential mechanical properties, including uniaxia...

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Main Authors: Seyed Morteza Davarpanah, Ákos Török, Balázs Vásárhelyi
Format: Article
Language:English
Published: Faculty of Mining, Geology and Petroleum Engineering 2022-01-01
Series:Rudarsko-geološko-naftni Zbornik
Subjects:
Online Access:https://hrcak.srce.hr/file/403549
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author Seyed Morteza Davarpanah
Ákos Török
Balázs Vásárhelyi
author_facet Seyed Morteza Davarpanah
Ákos Török
Balázs Vásárhelyi
author_sort Seyed Morteza Davarpanah
collection DOAJ
description The freezing technique has been employed for a long time to strengthen the mechanical properties of intact rock and rock mass; however, it has not received as much attention as it deserves. This paper thoroughly reviews the effect of freezing on the essential mechanical properties, including uniaxial compressive strength, tensile strength, and Young’s modulus. The laboratory tests include the determination of density, ultrasound speed propagation, and strength parameters such as uniaxial compressive strength, tensile strength, and Young’s modulus. According to previously published results, the strength of different rocks such as marl, limestone, sandstone, tuff, granite, and marble increased significantly due to freezing when the samples were tested in frozen conditions. However, there is variation in strength increase based on rock type. It is outlined here that freezing increases rock strength by a factor of 4 in porous rock and by a factor of 1.8 in crystalline rock. Additionally, Young’s modulus increases with a decrease in temperature; however, a further decrease in temperature from -10 to -20 °C has no effect on Young’s modulus. Moreover, mathematical modelling for frozen rock has been reviewed comprehensively. It was found that porosity, the density of rock grains, density of water, residual unfrozen water content, minimum unfrozen water content at freezing point, material parameters, the initial temperature of rock, crystal size, orientation and alignment of minerals, and the loading rate are the most critical parameters that influence frozen rock strength.
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spelling doaj.art-39e2532cd195428c9fa4c45f52fb62712023-09-03T07:48:46ZengFaculty of Mining, Geology and Petroleum EngineeringRudarsko-geološko-naftni Zbornik1849-04092022-01-013738396REVIEW ON THE MECHANICAL PROPERTIES OF FROZEN ROCKSSeyed Morteza Davarpanah0Ákos Török1Balázs Vásárhelyi2Department of Engineering Geology and Geotechnics, Faculty of Civil Engineering, Budapest University of Technology and EconomicsDepartment of Engineering Geology and Geotechnics, Faculty of Civil Engineering, Budapest University of Technology and EconomicsDepartment of Engineering Geology and Geotechnics, Faculty of Civil Engineering, Budapest University of Technology and EconomicsThe freezing technique has been employed for a long time to strengthen the mechanical properties of intact rock and rock mass; however, it has not received as much attention as it deserves. This paper thoroughly reviews the effect of freezing on the essential mechanical properties, including uniaxial compressive strength, tensile strength, and Young’s modulus. The laboratory tests include the determination of density, ultrasound speed propagation, and strength parameters such as uniaxial compressive strength, tensile strength, and Young’s modulus. According to previously published results, the strength of different rocks such as marl, limestone, sandstone, tuff, granite, and marble increased significantly due to freezing when the samples were tested in frozen conditions. However, there is variation in strength increase based on rock type. It is outlined here that freezing increases rock strength by a factor of 4 in porous rock and by a factor of 1.8 in crystalline rock. Additionally, Young’s modulus increases with a decrease in temperature; however, a further decrease in temperature from -10 to -20 °C has no effect on Young’s modulus. Moreover, mathematical modelling for frozen rock has been reviewed comprehensively. It was found that porosity, the density of rock grains, density of water, residual unfrozen water content, minimum unfrozen water content at freezing point, material parameters, the initial temperature of rock, crystal size, orientation and alignment of minerals, and the loading rate are the most critical parameters that influence frozen rock strength.https://hrcak.srce.hr/file/403549frozen rockstrength parametersYoung’s modulusmathematical modelling
spellingShingle Seyed Morteza Davarpanah
Ákos Török
Balázs Vásárhelyi
REVIEW ON THE MECHANICAL PROPERTIES OF FROZEN ROCKS
Rudarsko-geološko-naftni Zbornik
frozen rock
strength parameters
Young’s modulus
mathematical modelling
title REVIEW ON THE MECHANICAL PROPERTIES OF FROZEN ROCKS
title_full REVIEW ON THE MECHANICAL PROPERTIES OF FROZEN ROCKS
title_fullStr REVIEW ON THE MECHANICAL PROPERTIES OF FROZEN ROCKS
title_full_unstemmed REVIEW ON THE MECHANICAL PROPERTIES OF FROZEN ROCKS
title_short REVIEW ON THE MECHANICAL PROPERTIES OF FROZEN ROCKS
title_sort review on the mechanical properties of frozen rocks
topic frozen rock
strength parameters
Young’s modulus
mathematical modelling
url https://hrcak.srce.hr/file/403549
work_keys_str_mv AT seyedmortezadavarpanah reviewonthemechanicalpropertiesoffrozenrocks
AT akostorok reviewonthemechanicalpropertiesoffrozenrocks
AT balazsvasarhelyi reviewonthemechanicalpropertiesoffrozenrocks