2021
DOI: 10.1061/(asce)gt.1943-5606.0002626
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Modeling of Initial Stresses and Seepage for Large Deformation Finite-Element Simulation of Sensitive Clay Landslides

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Cited by 16 publications
(2 citation statements)
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“…where K 0 is the coefficient of static earth pressure, γ is the unit weight of the soil sample, and z is the depth. For sensitive clay, the values of K 0 always fall within the range of 0.5-1.5, with 0.5 often serving for K 0 in the case of Norwegian sensitive clays [35]. In this research, confining stresses are applied to the soil sample during the numerical MVST to represent the in situ confining stress state of soils under shallow seabed surfaces.…”
Section: Miniature Vane Shear Test Under Confining Stress Conditionsmentioning
confidence: 99%
“…where K 0 is the coefficient of static earth pressure, γ is the unit weight of the soil sample, and z is the depth. For sensitive clay, the values of K 0 always fall within the range of 0.5-1.5, with 0.5 often serving for K 0 in the case of Norwegian sensitive clays [35]. In this research, confining stresses are applied to the soil sample during the numerical MVST to represent the in situ confining stress state of soils under shallow seabed surfaces.…”
Section: Miniature Vane Shear Test Under Confining Stress Conditionsmentioning
confidence: 99%
“…Recently, multiple numerical methods have been developed and applied to investigate the postfailure processes of sensitive clay landslides. Examples include the coupled Eulerian-Lagrangian approach [11][12][13][14], the material point method, and the particle finite element method (PFEM) [15][16][17][18]. These studies primarily focused on upward landslides, particularly those indicating flow slide failures or spread failures due to toe erosion of the slope or seismic loading.…”
Section: Introductionmentioning
confidence: 99%