2018
DOI: 10.1016/j.sandf.2018.05.011
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Rate and acceleration effects on residual strength of kaolin and kaolin–bentonite mixtures in ring shearing

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Cited by 28 publications
(28 citation statements)
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“…Besides these effects, the behaviour of clays depends not only on the material state, but also on the strain amplitude. Researchers [6][7][8][9][10][11][12][13][14][15] have found that clays behave elastically only under very small strain amplitudes je 1 j\0:01 %. Under medium strain amplitudes 0:01 %\je 1 j\1 %, the so-called small strain effects, namely the stiffness increase due to reversal loading and the reduction in the plastic strain rate, take place.…”
Section: Introductionmentioning
confidence: 99%
“…Besides these effects, the behaviour of clays depends not only on the material state, but also on the strain amplitude. Researchers [6][7][8][9][10][11][12][13][14][15] have found that clays behave elastically only under very small strain amplitudes je 1 j\0:01 %. Under medium strain amplitudes 0:01 %\je 1 j\1 %, the so-called small strain effects, namely the stiffness increase due to reversal loading and the reduction in the plastic strain rate, take place.…”
Section: Introductionmentioning
confidence: 99%
“…e consolidation process would be finished until the end of the primary consolidation, which was confirmed by judgment based on the 3t-method [30,31]. e method has been widely used for the preparation of preconsolidation samples in the laboratory test in Japan [32][33][34]. After finishing the consolidation process in the tank, the vertical load was unloaded, and the cylindrical tank containing the sample was removed from the top and bottom plates.…”
Section: Methodsmentioning
confidence: 99%
“…Compared with reversal direct shear and triaxial compression tests, ring shear tests have been preferentially adopted to determine the residual shear strength of soil, due to their ability to shear unlimited displacements [6][7][8]. Many factors, such as shearing rate, moisture content, surface roughness, consolidated state, and temperature, affect the magnitude of the residual soil strength [9][10][11][12][13][14][15][16]. Among these factors, the loss of strength caused by the shearing rate (greater than 100 mm/min) explains the high acquired velocity of landslides [17,18].…”
Section: Introductionmentioning
confidence: 99%
“…10 Geofluids 300 kPa and shearing rate of 393 mm/min). The mean size (D 50 ) decreased from 14.51 μm (original sample) to 11.68 μm (sample with a normal stress of 300 kPa and shearing rate of 393 mm/min).4.5.2.…”
mentioning
confidence: 99%