2018
DOI: 10.1002/nme.5921
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Generalized radial‐return mapping algorithm for anisotropic von Mises plasticity framed in material eigenspace

Abstract: A computationally efficient integration algorithm for anisotropic plasticity is proposed, which is identified as a generalization of the radial-return mapping algorithm to anisotropy. The algorithm is based upon formulation within the eigenspace of a material anisotropy tensor associated with anisotropic quadratic von Mises (J 2 ) plasticity (also called Hill plasticity), for which it is shown to ensure that the flow rule remains associative, ie, the normality condition is satisfied. Extension of the algorithm… Show more

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Cited by 11 publications
(9 citation statements)
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“…Using Eq. 3.9, one can define anisotropic creep compliance and anisotropic plastic yield surfaces [8,9,10]. Within the report [11], the following activities were carried out:…”
Section: Methodsmentioning
confidence: 99%
“…Using Eq. 3.9, one can define anisotropic creep compliance and anisotropic plastic yield surfaces [8,9,10]. Within the report [11], the following activities were carried out:…”
Section: Methodsmentioning
confidence: 99%
“…Here, 𝜎 𝑑 𝑢,1 and 𝜎 𝑑 𝑢,3 are the across-and along-column yield stresses, in compression mode, respectively. 101 We adopt the Hill plasticity-type yield function to describe the anisotropy of ice 105 as follows:…”
Section: Free Energy Specificationmentioning
confidence: 99%
“…we adopt a projection-based technique that introduces orientation-dependent strain measures in a projected space to replace the strain invariants as variables for the hyperelasticity functional and the yield surface. [31][32][33][34][35][36] In the elastic regime (see Section 2.1, a hyperelastic model for soil originally proposed to capture the pressure-dependent elasticity of clay (cf. Refs.…”
Section: Constitutive Laws For Saturation-dependent Anisotropy In Fro...mentioning
confidence: 99%
“…To phenomenologically replicate the transversely isotropic response of the freezing soil, we introduce both a transversely isotropic hyperelasticity energy function and a transversely isotropic critical state plasticity model of which the degree of anisotropy is dictated by the degree of saturation of ice. we adopt a projection‐based technique that introduces orientation‐dependent strain measures in a projected space to replace the strain invariants as variables for the hyperelasticity functional and the yield surface 31–36 …”
Section: Constitutive Laws For Saturation‐dependent Anisotropy In Fro...mentioning
confidence: 99%