Résumé
A planar crack generically segments into an array of "daughter cracks" shaped as tilted facets when loaded with both a tensile stress normal to the crack plane (mode I) and a shear stress parallel to the crack front (mode III). We investigate facet propagation and coarsening using in situ microscopy observations of fracture surfaces at different stages of quasistatic mixed-mode crack propagation and phase-field simulations. The results demonstrate that the bifurcation from propagating a planar to segmented crack front is strongly subcritical, reconciling previous theoretical predictions of linear stability analysis with experimental observations. They further show that facet coarsening is a self-similar process driven by a spatial period-doubling instability of facet arrays.
| langue originale | Anglais |
|---|---|
| Numéro d'article | 265503 |
| journal | Physical Review Letters |
| Volume | 115 |
| Numéro de publication | 26 |
| Les DOIs | |
| état | Publié - 30 déc. 2015 |
| Modification externe | Oui |
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