2019
DOI: 10.1016/j.ijrmms.2019.104090
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Assessing the effect of freezing-thawing cycles on the results of the triaxial compressive strength test for calc-schist rock

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Cited by 69 publications
(26 citation statements)
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“…Moreover, many research investigations generally indicate that increasing the number of freeze–thaw cycles decreases the uniaxial compressive strength, tensile strength, dry density and P-wave velocity of rocks, while the water absorption and porosity of rocks increase 9 11 . Seyed et al and Yu et al conducted triaxial compression tests on frozen-thawed rocks and found that the cohesion and internal friction angle of rocks decreased exponentially with the increase of the number of freeze–thaw cycles 4 , 12 . They found that the correlation between rock compressive strength, confining pressure and cycles can be described by the Mohr–Coulomb strength criterion 13 .…”
Section: Introductionmentioning
confidence: 99%
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“…Moreover, many research investigations generally indicate that increasing the number of freeze–thaw cycles decreases the uniaxial compressive strength, tensile strength, dry density and P-wave velocity of rocks, while the water absorption and porosity of rocks increase 9 11 . Seyed et al and Yu et al conducted triaxial compression tests on frozen-thawed rocks and found that the cohesion and internal friction angle of rocks decreased exponentially with the increase of the number of freeze–thaw cycles 4 , 12 . They found that the correlation between rock compressive strength, confining pressure and cycles can be described by the Mohr–Coulomb strength criterion 13 .…”
Section: Introductionmentioning
confidence: 99%
“…Additionally, the pore structure of rock under freeze–thaw can be observed using scanning electron microscopy (SEM). The existing research generally indicates that the pores of the rock expand and the particles fall off with the increase of freeze–thaw number 2 , 12 , 24 26 . However, due to the extremely complex pore structure characteristics of rock, there is little research on quantitative analysis of microstructure changes after rock freeze–thaw damage.…”
Section: Introductionmentioning
confidence: 99%
“…Liu et al [11] improved an empirical equation to determine the uniaxial compressive strength of rocks subjected to freeze-thaw cycles based on a fatigue damage model. Fu et al [12] and Seyed Mousavi et al [13] proposed a TCS prediction model for transversely isotropic rocks subjected to freeze-thaw cycles based on the single discontinuity theory. However, the unknown parameters in those models should be determined by experimental tests.…”
Section: Introductionmentioning
confidence: 99%
“…China is one of the countries with the largest cold region distribution, accounting for about 75% of the total land area of the country, where an increasing number of rock mass projects have been launched in cold regions driven by national policies in recent years [1][2][3][4]. In cold regions, the macroscopic damage, frost heave failure, and instability caused by the freezing-thawing cycle of fissure water under alternating temperature changes are considered as the main weathering process of rock mass [5][6][7], which has a decisive influence on the stability of rock mass [8][9][10][11]. Therefore, the researches on the mechanism of damage and degradation of rock mass under the freezing-thawing cycle condition are of great significance for engineering construction in cold regions [12][13][14], which have attracted the attention of numerous experts and scholars [15][16][17].…”
Section: Introductionmentioning
confidence: 99%