Quasi-static hydraulic crack growth driven by Darcy's law

dc.contributor.areaMathematicsen_US
dc.contributor.authorAlmi, Stefano
dc.date.accessioned2016-06-23T09:18:19Z
dc.date.available2016-06-23T09:18:19Z
dc.date.issued2016
dc.description.abstractIn the framework of rate independent processes, we present a variational model of quasi-static crack growth in hydraulic fracture. We first introduce the energy functional and study the equilibrium conditions of an unbounded linearly elastic body subject to a remote strain ε ∈ R and with a sufficiently regular crack Γ filled by a volume V of incompressible fluid. In particular, we are able to find the pressure p of the fluid inside the crack as a function of Γ, V , and ε. Then, we study the problem of quasi-static evolution for our model, imposing that the fluid volume V and the fluid pressure p are related by Darcy’s law. We show the existence of such an evolution, and we prove that it satisfies a weak notion of the so-called Griffith’s criterion.en_US
dc.identifier.urihttps://openscience.sissa.it/handle/1963/35198
dc.language.isoenen_US
dc.miur.area1en_US
dc.relation.ispartofseriesSISSA;29/2016/MATE
dc.subjectvariational models, free-discontinuity problems, crack propagation, brittle fractures, hydraulic fractures, quasi-static evolution, energy release rate, Griffith’s criterionen_US
dc.subject.miurMAT/05en_US
dc.titleQuasi-static hydraulic crack growth driven by Darcy's lawen_US
dc.typePreprinten_US
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