2020
DOI: 10.1007/s00161-020-00885-1
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A thermodynamically consistent framework for visco-elasto-plastic creep and anisotropic damage in saturated frozen soils

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Cited by 10 publications
(3 citation statements)
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“…On short term behaviour, extensive laboratory investigations have shown that the mechanical behaviour of clay rocks can be characterised by coupled plastic damage 11 . Concerning long term behaviour, time‐dependent creep deformation constitutes another important feature of clay rocks 3,12–15 . Classically, the time‐dependent inelastic deformation of a material is described by phenomenological viscoplastic models (e.g., Bui et al 16 …”
Section: Introductionmentioning
confidence: 99%
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“…On short term behaviour, extensive laboratory investigations have shown that the mechanical behaviour of clay rocks can be characterised by coupled plastic damage 11 . Concerning long term behaviour, time‐dependent creep deformation constitutes another important feature of clay rocks 3,12–15 . Classically, the time‐dependent inelastic deformation of a material is described by phenomenological viscoplastic models (e.g., Bui et al 16 …”
Section: Introductionmentioning
confidence: 99%
“…11 Concerning long term behaviour, time-dependent creep deformation constitutes another important feature of clay rocks. 3,[12][13][14][15] Classically, the time-dependent inelastic deformation of a material is described by phenomenological viscoplastic models (e.g., Bui et al 16 ; Sun et al 17 ). Although these models provide efficient mathematical tools for the long-term analyses of structures, the physical mechanisms of creep deformation are not explicitly considered.…”
Section: Introductionmentioning
confidence: 99%
“…As a typical representative of deep foundation, pile foundation stand out as a quintessential choice and find wide applications in multifarious complex foundation scenarios. In challenging geological areas, such as collapsible soil 2 , expansive soil 3 , frozen soil 4 , the stress relationship between pile and soil will change with the change of soil engineering properties. Frozen soil, in particular, represents an anisotropic, heterogeneous, multiphase complexity, which is composed of solid soil particles, liquid water, gas and ice.…”
Section: Introductionmentioning
confidence: 99%