2020
DOI: 10.1016/j.cscm.2020.e00441
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Relationship between the matric suction and the shear strength in unsaturated soil

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Cited by 24 publications
(7 citation statements)
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“…In the case of expansive soils, these changes in moisture content mostly occur due to seasonal fluctuations. As a consequence, the expansive soil experiences either settlement or ground heave due to wetting and drying [1][2][3][4], and as a result of increased moisture content induced by water infiltration, the shear strength of unsaturated soil begins to decrease as the negative pore water pressure increases, which is one of the cause of slope instability [5][6][7]. The investigation of the impact of moisture content fluctuations caused by infiltration on the mechanical properties of unsaturated soil and its implications for the stability of structural foundations has become a prominent area of interest in civil and geomechanical research [8][9][10][11][12][13][14][15][16].…”
Section: Introductionmentioning
confidence: 99%
“…In the case of expansive soils, these changes in moisture content mostly occur due to seasonal fluctuations. As a consequence, the expansive soil experiences either settlement or ground heave due to wetting and drying [1][2][3][4], and as a result of increased moisture content induced by water infiltration, the shear strength of unsaturated soil begins to decrease as the negative pore water pressure increases, which is one of the cause of slope instability [5][6][7]. The investigation of the impact of moisture content fluctuations caused by infiltration on the mechanical properties of unsaturated soil and its implications for the stability of structural foundations has become a prominent area of interest in civil and geomechanical research [8][9][10][11][12][13][14][15][16].…”
Section: Introductionmentioning
confidence: 99%
“…The soil-water retention curve (SWRC), defines the relationship between soil suction and its water content [10][11][12][13]. The creation SWRCs enable the geotechnical experts to characterize the suction behavior of unsaturated soil and effectively address the diverse geotechnical engineering challenges related to slope stability, foundation bearing capacity, seepage, permeability, and shear strength properties of unsaturated soil [14][15][16][17]. While significant advances have been made in the field of unsaturated soil mechanics in recent years, there is still a notable gap in our understanding of the unsaturated water retention behavior of cementitious stabilized soil, especially in gypseous soil.…”
Section: Introductionmentioning
confidence: 99%
“…Chen et al [7,8] indicated that the in situ stress state of natural soil is usually inherently anisotropic, that is to say, the static lateral pressure coefficient K 0 ≠ 1 in the actual stress state of soil. Fattah et al [9][10][11][12] studied the shear strength properties for unsaturated soil with different matric suction values, and it is concluded that the matric suction is considered an important contributor to unsaturated shear strength properties. Wang [13] and Wen et al [5] derived the critical edge load of soft soil foundation with hard crust based on Mohr-Coulomb criterion, the results take no account of intermediate principal stress, and the assumption K 0 = 1 is inconsistent with the actual stress state of soil.…”
Section: Introductionmentioning
confidence: 99%