We study an evolution model for fractured elastic materials in the 2-dimensional case, for which the crack path is not assumed to be known a priori. We introduce some general assumptions on the structure of the fracture sets suitable to remove the restrictions on the regularity of the crack sets and to allow for kinking and branching to develop. In addition we define the front of the fracture and its velocity. By means of a time-discretization approach, we prove the existence of a continuous-time evolution that satisfies an energy inequality and a stability criterion. The energy balance also takes into account the energy dissipated at the front of the fracture. The stability criterion is stated in the framework of Griffith's theory, in terms of the energy release rate, when the crack grows at least at one point of its front.

%B Asymptotic Analysis %I SISSA %V 89 %P 63-110 %G en %U https://content.iospress.com/articles/asymptotic-analysis/asy1233 %N 1-2 %9 Research Article %1 6293 %2 Mathematics %4 1 %# MAT/05 ANALISI MATEMATICA %$ Submitted by Simone Racca (sracca@sissa.it) on 2012-12-27T14:51:21Z\\nNo. of bitstreams: 1\\nA model for crack growth with branching and kinking - Racca.pdf: 566327 bytes, checksum: c6cfc3165c0bfee387a9c6f8b1e5b4b1 (MD5) %& 63 %R 10.3233/ASY-141233 %0 Journal Article %D 2014 %T A variational model for the quasi-static growth of fractional dimensional brittle fractures %A Simone Racca %A Rodica Toader %K Variational models %XWe propose a variational model for the irreversible quasi-static evolution of brittle fractures having fractional Hausdorff dimension in the setting of two-dimensional antiplane and plane elasticity. The evolution along such irregular crack paths can be obtained as $\Gamma$-limit of evolutions along one-dimensional cracks when the fracture toughness tends to zero.

%I European Mathematical Society %G en %U http://hdl.handle.net/1963/6983 %1 6973 %2 Mathematics %4 -1 %$ Submitted by Simone Racca (sracca@sissa.it) on 2013-07-18T08:39:00Z No. of bitstreams: 1 Racca_Toader.pdf: 416939 bytes, checksum: cf459548a10944037e56b7504fe60f51 (MD5) %R 10.4171/IFB/328 %0 Thesis %D 2013 %T Some models of crack growth in brittle materials %A Simone Racca %K Quasi-static crack evolution %I SISSA %G en %1 7205 %2 Mathematics %4 1 %# MAT/05 ANALISI MATEMATICA %$ Submitted by Simone Racca (sracca@sissa.it) on 2013-10-23T13:11:13Z No. of bitstreams: 1 Racca_PhDThesis.pdf: 1710871 bytes, checksum: ea174e98f8849253e71cdefa52c6c8b8 (MD5) %] Introduction Chapter 1. Preliminaries Chapter 2. A viscosity-driven crack evolution Chapter 3.A variational model for the quasi-static growth of fractional dimensional brittle fractures Chapter 4. A model for crack growth with branching and kinking Bibliography %0 Journal Article %J Advances in Calculus of Variations 5 (2012) 433-483 %D 2012 %T A Viscosity-driven crack evolution %A Simone Racca %XWe present a model of crack growth in brittle materials which couples dissipative effects on the crack tip and viscous effects. We consider the 2 -dimensional antiplane case with pre-assigned crack path, and firstly prove an existence result for a rate-dependent evolution problem by means of time-discretization. The next goal is to describe the rate-independent evolution as limit of the rate-dependent ones when the dissipative and viscous effects vanish. The rate-independent evolution satisfies a Griffithâ€™s criterion for the crack growth, but, in general, it does not fulfil a global minimality condition; its fracture set may exhibit jump discontinuities with respect to time. Under suitable regularity assumptions, the quasi-static crack growth is described by solving a finite-dimensional problem.

%B Advances in Calculus of Variations 5 (2012) 433-483 %I SISSA %G en %U http://hdl.handle.net/1963/5130 %1 4944 %2 Mathematics %3 Functional Analysis and Applications %4 -1 %$ Submitted by Maria Pia Calandra (calapia@sissa.it) on 2011-11-29T07:47:42Z\\r\\nNo. of bitstreams: 1\\r\\n63M_Racca.pdf: 473110 bytes, checksum: f4d49c3f7e2b984e9694fbd66a806447 (MD5) %R 10.1515/acv-2011-0012