2016
DOI: 10.1051/e3sconf/20160914018
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Characterizing the variation of small strain shear modulus for silt and sand during hydraulic hysteresis

Abstract: Abstract. Experimental studies have indicated that the small strain shear modulus, Gmax, of unsaturated silt and clay has a greater amount during imbibition than during drainage, when presented as a function of matric suction. However, due to material properties and inter-particle forces, different behavior is expected in the case of sand. Although considerable research has been devoted in recent years to characterize the behaviour of Gmax of sand during drainage, rather less attention has been paid to the eff… Show more

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Cited by 12 publications
(3 citation statements)
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“…However, the shear modulus relation might be different depending on the effective stress formula, strain level, and also testing method. For example, Ghayoomi et al (2017) used triaxial test, or Khosravi et al (2016) used resonant column test to show that still there would be meaningful increase in normalized modulus (or constant effective stress modulus) by increasing the suction or change of the degree of saturation. Considering the suction dependency of the shear modulus, in addition to the previously known affecting parameters, such as the effective stress, the void ratio, OCR, and the shear strain, an additional term could be included in…”
Section: Fig 12mentioning
confidence: 99%
“…However, the shear modulus relation might be different depending on the effective stress formula, strain level, and also testing method. For example, Ghayoomi et al (2017) used triaxial test, or Khosravi et al (2016) used resonant column test to show that still there would be meaningful increase in normalized modulus (or constant effective stress modulus) by increasing the suction or change of the degree of saturation. Considering the suction dependency of the shear modulus, in addition to the previously known affecting parameters, such as the effective stress, the void ratio, OCR, and the shear strain, an additional term could be included in…”
Section: Fig 12mentioning
confidence: 99%
“…Since the degree of saturation along a drying path is higher than the degree of saturation along a wetting path, one would expect G to be higher along a drying path. Although an evidence of this has been observed experimentally [23], a number of experimental investigations show an opposite trend, i.e., the soil is observed to be significantly stiffer along a wetting path [24,40]. Inspection of experimental data also reveals that the change of G with suction or degree of saturation occurs in either a monotonic or non-monotonic fashion [23,45].…”
Section: Micromechanical Modelling Of Unsaturated Soilsmentioning
confidence: 86%
“…Although an evidence of this has been observed experimentally [23], a number of experimental investigations show an opposite trend, i.e., the soil is observed to be significantly stiffer along a wetting path [24,40]. Inspection of experimental data also reveals that the change of G with suction or degree of saturation occurs in either a monotonic or non-monotonic fashion [23,45]. Ideally, a stiffness model should be capable of capturing the physics behind the two observed behaviours.…”
Section: Micromechanical Modelling Of Unsaturated Soilsmentioning
confidence: 92%