Experimental investigation on mechanical properties and strength criteria of frozen soft rock

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Yayımlandı:PLoS One vol. 20, no. 1 (Jan 2025), p. e0313493
Yazar: Wang, Zhenhua
Diğer Yazarlar: Wang, Zecheng, Dongwei Li Zhiwen Jia Xiqi Liu
Baskı/Yayın Bilgisi:
Public Library of Science
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100 1 |a Wang, Zhenhua 
245 1 |a Experimental investigation on mechanical properties and strength criteria of frozen soft rock 
260 |b Public Library of Science  |c Jan 2025 
513 |a Journal Article 
520 3 |a Excavation of underground engineering structures involving deeply buried water-rich soft rocks is generally carried out using the artificial freezing method. A series of undrained uniaxial and triaxial shear and creep tests were conducted on soft rocks under different confining pressures (0, 0.2, 0.5, and 1.0 MPa) at different freezing temperatures (room temperature, -5°C, -10°C, and -15°C). Test results indicate that the frozen soft rocks show strain softening characteristics. The stress—strain curve changes from a straight line to a curve as deviatoric stress constantly increases, while it decreases abruptly after the deviatoric stress reaches the peak and is slightly affected by the freezing temperature. At the same temperature, shear strength increases at a rate of 5.6 MPa/°C with increasing confining pressure; as freezing temperature decreases, the shear strength increases at 0.34 MPa/°C, and cohesion increases at 0.6 MPa/°C. Under the same confining pressure, the failure strain of soft rock decreases with the decrease of temperature. The Mohr-Coulomb (M-C) criterion can accurately describe the failure process of frozen soft rocks in the pre-peak stage, with a correlation coefficient greater than 0.98. Within the test stress range, soft rocks display attenuated stable creep deformation. Acoustic emission (AE) tests were conducted to further verify that the soft rocks show shear failure under load, with a shear plane showing an angle of 45° with the horizontal. The research findings provide technical support and theoretical reference for studying rock mechanical properties as well as for designing and carrying out underground freezing of rocks in a low-temperature environment. 
653 |a Mechanical properties 
653 |a Plastic deformation 
653 |a Creep strength 
653 |a Creep tests 
653 |a Underground structures 
653 |a Freezing 
653 |a Low temperature environments 
653 |a Room temperature 
653 |a Low temperature 
653 |a Excavation 
653 |a Rocks 
653 |a Rock excavation 
653 |a Buried structures 
653 |a Freezing temperatures 
653 |a Correlation coefficient 
653 |a Correlation coefficients 
653 |a Confining 
653 |a Shear tests 
653 |a Shear strength 
653 |a Acoustic emission 
653 |a Soil mechanics 
653 |a Temperature 
653 |a Failure 
653 |a Mohr-Coulomb theory 
653 |a Acoustic emission testing 
653 |a Shear planes 
653 |a Straight lines 
653 |a Deformation 
653 |a Strain 
653 |a Environmental 
700 1 |a Wang, Zecheng 
700 1 |a Dongwei Li Zhiwen Jia Xiqi Liu 
773 0 |t PLoS One  |g vol. 20, no. 1 (Jan 2025), p. e0313493 
786 0 |d ProQuest  |t Health & Medical Collection 
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