Issue 19
K. Pham et alii, Frattura ed Integrità Strutturale, 19 (2012) 5-19; DOI: 10.3221/IGF-ESIS.19.01 15 Figure 4 : Damage profile in the localization zone when the bar breaks, for = 4 q and different values of the parameter p ( = 1/ 2,1, 2, 4 p ) in the family of brittle materials of Example 1. Figure 5 : The damage profile for a given t and its evolution with t by assuming that t t is decreasing in the case of the model of Example 1 with = 2 p and = 4 q . The rupture occurs when = 0 t and ( ) = 1 t . We check numerically that ( ) D is decreasing. It is easy to check that ( ) d is decreasing with ( ) = 0 d c while (0) d represents the dissipated energy in a localization zone during to the process of damage up to the rupture. Let us call fracture energy and denote by c G this energy by reference to the Griffith surface energy density in Griffith theory of fracture. Since (0) =1 , we have Property 6 (Fracture energy) The dissipated energy in an inner localization zone during the damage process up to the rupture is a material constant c G which is given by 1 0 0 = 8 ( ) c G E w d (34) Because of the lack of constraint on the damage at the boundary, the dissipated energy in a boundary localization zone up to the rupture is / 2 c G . Example 6 In the case of the family of strongly materials of Example 1 the fracture energy is given by 1 0 = 2 , = 1 p c p c p q G J J v dv p (35) Thus c G is proportional to the product of the critical stress by the internal length, the coefficient of proportionality depending on the exponents p and q . The force-displacement relation The time is fixed and we still omit the index t . Let U be the prescribed displacement, = / U L the average strain and the stress in the bar which contains 1 n localization zones. Using (11), recalling that = 0 outside the localization zones and that all localization zones have the same size 2 ( ) D and the same profile, we get
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