2004
DOI: 10.1016/j.cma.2003.12.067
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Cam-Clay plasticity. Part V: A mathematical framework for three-phase deformation and strain localization analyses of partially saturated porous media

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Cited by 242 publications
(208 citation statements)
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“…local level). This is the common procedure used in the literature for finite element analysis involving unsaturated soils [5,38,43], because these two increments (i.e. , s) can be easily approximated at the corresponding integration points, once the nodal displacements and pore fluid pressures increments have been found from the discretized global equations.…”
Section: Initial Statementioning
confidence: 99%
“…local level). This is the common procedure used in the literature for finite element analysis involving unsaturated soils [5,38,43], because these two increments (i.e. , s) can be easily approximated at the corresponding integration points, once the nodal displacements and pore fluid pressures increments have been found from the discretized global equations.…”
Section: Initial Statementioning
confidence: 99%
“…The authors have not been able to identify any existing analytical solutions for inception of strain localization in unsaturated soils. Borja (2004) developed a mathematical framework for numerical analysis of three-phase deformation and strain localization of partially saturated porous media. The framework was used to detect the onset of strain localization for plane strain compression at the constitutive level.…”
Section: Introductionmentioning
confidence: 99%
“…The framework was used to detect the onset of strain localization for plane strain compression at the constitutive level. Borja (2004) used the degree of saturation as the effective stress parameter. Schiava and Etse (2006) conducted a numerical assessment of strain localization in unsaturated soils at constant suction.…”
Section: Introductionmentioning
confidence: 99%
“…Also all the following equations are written in isothermal conditions, which evidently leads to not considering the temperature gradient and limits the modelling of the evaporation (Gawin, Sanavia, & Schrefle, 1998). If the water is assumed incompressible, the balance of water mass is (Borja, 2004):…”
Section: Approach To Model Slope Response To Rainfallmentioning
confidence: 99%