Abstract:The fluctuation of mechanical fields arising in polycrystals is investigated. These materials are viewed as composites of the Hashin-Shtrikman type with a large number of anisotropic phases and a 'granular' topology. We show that the estimation of the intra-phase stress and strain (rate) second moments comes down to the resolution of a linear system of equations. Applied to a linear viscous face-centred cubic (FCC) polycrystal, it is observed that significant local slip rates are estimated even when the corres… Show more
“…One well known limitation of such modeling is the absence of non linear response under hydrostatic stress (see Weng, 1992, 1993 for a discussion on this issue in elasto-plasticity). The definition of better reference moduli is still an active research subject in the literature, an interesting approach being the use of the second-order moment of strain in order to better take into account the non-uniformity of the strain field (see Hu (1996), Brenner et al (2004), González et al (2004) and Ponte Castañ eda (2002) for a variational approach).…”
Section: Definition Of Reference Constitutive Modulimentioning
“…One well known limitation of such modeling is the absence of non linear response under hydrostatic stress (see Weng, 1992, 1993 for a discussion on this issue in elasto-plasticity). The definition of better reference moduli is still an active research subject in the literature, an interesting approach being the use of the second-order moment of strain in order to better take into account the non-uniformity of the strain field (see Hu (1996), Brenner et al (2004), González et al (2004) and Ponte Castañ eda (2002) for a variational approach).…”
Section: Definition Of Reference Constitutive Modulimentioning
“…C el r can then be computed analytically. Otherwise, if the inclusions are not spheroids or E is computed with an anisotropic matrix's modulus tensor, then the partial derivatives can be approximated numerically, as in Brenner et al (2004).…”
Section: Elastic Predictor In Each Phasementioning
“…The SC scheme is therefore especially appropriate for polycrystals. The expression of the stress localization tensor in a general context of anisotropy is given, e.g., by Brenner et al [2004].…”
Section: A1 Exact Solution For Linear Elastoviscoplasticitymentioning
confidence: 99%
“…It must be made clear, however, that long-range interactions associated with spatial correlations between dislocation avalanches are not considered owing to the simplicity of the adopted local constitutive relation (5). For purely elastic and purely viscoplastic regime, the standard deviations (8) can be calculated by an appropriate differentiation of the corresponding effective potential [Brenner et al, 2004].…”
[1] A salient feature of the rheology of isotropic polycrystalline ices is the decrease of the strain rate by more than 2 orders of magnitude during transient creep tests to reach a secondary creep regime at a strain which is systematically of $1%. We use a recent (socalled ''affine'') version of the self-consistent mean-field theory to model the elastoviscoplastic behavior of ice. The model aims at bridging scales between the rheology of single grain and the one of polycrystals by evaluating the intergranular interactions. It takes into account the long-term memory effects, which manifests itself by the fact that local stress and strain rate in grains depend on the whole mechanical history of the polycrystal. It is shown that the strong hardening amplitude during the transient creep is entirely explained by the stress redistribution within the specimen, from an almost uniform stress distribution upon instantaneous loading (purely elastic response) to strong interphase and intraphase heterogeneities in the stationary regime (purely viscoplastic response). The experimental hardening kinetic is much too slow to be explained by the same process; it is attributed to the hardening of hard glide slip systems (prismatic slip) in the transient regime. Moreover, the model very well reproduces the permanent creep rate of several highly anisotropic specimens of the Greenland Ice Core Project ice core (pronounced crystallographic textures), when accounting for a single-grain rheology that well matches the experimental one. Our results are consistent with recent findings concerning dislocation dynamics in ice.
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