2018
DOI: 10.1016/j.enggeo.2018.03.033
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The impact of environmental temperature change on the interior temperature of quasi-sandstone in cold region: Experiment and numerical simulation

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Cited by 36 publications
(9 citation statements)
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“…Using a similar material to simulate the joint, a direct shear test was performed and the entire shear stress-shear displacement curve was recorded under a certain normal load [9,[37][38][39][40][41][42][43]. e white Portland cement numbered 425 and Advances in Civil Engineering muddy river sand with a particle size of 0.5 to 1.0 mm are used for sampling and then casted according to the ratio (mass ratio) cement : sand : water � 1 : 0.53 : 0.45 with the size of 150 × 150 × 120 mm.…”
Section: Sample Preparation and Test Methodsmentioning
confidence: 99%
“…Using a similar material to simulate the joint, a direct shear test was performed and the entire shear stress-shear displacement curve was recorded under a certain normal load [9,[37][38][39][40][41][42][43]. e white Portland cement numbered 425 and Advances in Civil Engineering muddy river sand with a particle size of 0.5 to 1.0 mm are used for sampling and then casted according to the ratio (mass ratio) cement : sand : water � 1 : 0.53 : 0.45 with the size of 150 × 150 × 120 mm.…”
Section: Sample Preparation and Test Methodsmentioning
confidence: 99%
“…It can be speculated that the densification of marble is the largest among the three kinds of rock. After performing basic physical and mechanical testing, the density of the marble, granite, and sandstone is 2.75, 2.55, and 2.35 g/cm 3 , respectively. The porosity of Three typical rocks of marble, granite, and sandstone were prepared to conduct the frost heaving force measurement testing.…”
Section: Methodsmentioning
confidence: 99%
“…In cold regions, the freeze-thaw (F-T) actions within the preexisting discontinuous (e.g., bedding planes, interbeds, cracks, foliation, flaw, and fault) would lead to the instability and damage of rock, such as avalanche, collapses, rock falling, and landslides [1][2][3][4][5][6]. Water from the thawing of snow or sleet penetrates those rock discontinuities, and freeze occurs when the temperature is below zero and the frost heaving force produces within the preexisting fractures or discontinuities.…”
Section: Introductionmentioning
confidence: 99%
“…Rock joints widely exist in rock engineering [1][2][3][4]. e mechanical properties of rock joints are considered as the controlling factors of rock mass engineering stability [5][6][7][8].…”
Section: Introductionmentioning
confidence: 99%