2017
DOI: 10.1016/j.compgeo.2016.08.004
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An elastoviscoplastic constitutive model for geomaterials: Application to hydromechanical modelling of claystone response to drift excavation

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Cited by 20 publications
(8 citation statements)
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“…From the mathematical point of view, e, p, s, and X are order 2 symmetrical tensors which can be identified with 3 Â 3 symmetrical matrices after the choice of an orthonormal basis. In other words, those tensors will be considered as elements of M 3 s . The plasticity (or yield) criterion is defined by giving the (closed with non-empty interior) convex set K of M 3 s where the thermodynamical forces X must lie.…”
Section: The Dissipation Potential or Equivalently The Convex Setmentioning
confidence: 99%
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“…From the mathematical point of view, e, p, s, and X are order 2 symmetrical tensors which can be identified with 3 Â 3 symmetrical matrices after the choice of an orthonormal basis. In other words, those tensors will be considered as elements of M 3 s . The plasticity (or yield) criterion is defined by giving the (closed with non-empty interior) convex set K of M 3 s where the thermodynamical forces X must lie.…”
Section: The Dissipation Potential or Equivalently The Convex Setmentioning
confidence: 99%
“…(However, we will see in the next section that the image of this domain in the stress space evolves with the plastic strain.) In practice, the convex K is characterized by a convex function f : M 3 S ↦ ℝ so that the plasticity criterion reads as…”
Section: The Dissipation Potential or Equivalently The Convex Setmentioning
confidence: 99%
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