2006
DOI: 10.1016/j.crme.2006.11.005
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Résistance d'un polycristal avec interfaces intergranulaires imparfaites

Abstract: On s'intéresse à un polycristal poreux constitué de grains en contact le long d'interfaces. On met tout d'abord en oeuvre un schéma autocohérent faisant intervenir des pores sphériques ainsi qu'un motif constitué d'un noyau élastique entouré d'une interface également élastique. On établit ensuite une formule permettant de déterminer la moyenne quadratique de la discontinuité de déplacement tangentiel dans les interfaces entre grains. Dans la dernière partie, on applique la méthode sécante modifiée pour détermi… Show more

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Cited by 24 publications
(22 citation statements)
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“…Still, in the maximally stressed bundle, not the (first-order) average phase stresses r hyd;u;J ; as introduced below (8), but stress peaks govern the failure of the (u,0)-oriented hydrate phase [61]. Such peaks can be appropriately estimated through quadratic stress averages over suitably chosen subdomains of the RVE sc , such as 3D subdomains (bulk phases) [4,38,49] or 2D interfaces [15,20]. We here introduce quadratic (or second-order) averages over (u,0)-oriented hydrates, averaged, in the sense of (4), over all hydrates oriented in one direction (u,0), max x2X hyd;u;J r dev ðx; u; JÞ % r dev hyd;u;J ¼ lim…”
Section: Upscaling Of Strength From Hydrate Level To Shotcrete Levelmentioning
confidence: 99%
“…Still, in the maximally stressed bundle, not the (first-order) average phase stresses r hyd;u;J ; as introduced below (8), but stress peaks govern the failure of the (u,0)-oriented hydrate phase [61]. Such peaks can be appropriately estimated through quadratic stress averages over suitably chosen subdomains of the RVE sc , such as 3D subdomains (bulk phases) [4,38,49] or 2D interfaces [15,20]. We here introduce quadratic (or second-order) averages over (u,0)-oriented hydrates, averaged, in the sense of (4), over all hydrates oriented in one direction (u,0), max x2X hyd;u;J r dev ðx; u; JÞ % r dev hyd;u;J ¼ lim…”
Section: Upscaling Of Strength From Hydrate Level To Shotcrete Levelmentioning
confidence: 99%
“…For further use, the quadratic average of the tangential part of the stress vector acting at grain contacts of the non‐coated grains, excluding once again the interface between the grains and the porous phase, also needs to be calculated. As shown in , adapting to the case of a REV containing elastic interfaces a method presented in , this average trueTt2¯Q can be deduced by differentiation of the macroscopic energy: Tt2true¯Q=khom1RkitalictQ1Σm2+ghom1RkitalictQ1Σd23fQ()fQ+fC()2fQ+2fC1where Σd=ΣΣm1:ΣΣm1/2.…”
Section: Effective Friction Coefficient Of a Clayey Sand Gougementioning
confidence: 99%
“…In turn, the non linear problem can be solved using secant or affine methods (Suquet, 1995(Suquet, , 1997 which rely on the solution to the associated linear problem. These methods proved successful to predict the strength of heterogeneous material, even in the presence of interface effects (Barth el emy, 2005; Barth el emy and Dormieux, 2004;Dormieux et al, 2010Dormieux et al, , 2006Dormieux et al, . 2007He et al, 2013;Maalej et al, 2009;Maghous et al, 2009;Sanahuja and Dormieux, 2005).…”
Section: Introductionmentioning
confidence: 96%
“…Such imperfect interfaces can be characterized by a criterion the stress vector acting on the interface must not exceed. Thanks to homogenization methods, the strength of granular geomaterials has been investigated, successively considering the cases of rigid grains interfaced by a Tresca criterion (Dormieux et al, 2007), a2 frictional criterion (Maalej et al, 2009) or a cohesive frictional criterion (He et al, 2013), as well as the competition between Tresca interfacial and Von Mises intragranular strength (Dormieux et al, 2010).…”
Section: Introductionmentioning
confidence: 99%