A Direct Derivation of the Griffith-Irwin Relationship using a Crack tip Unloading Stress Wave Model

dc.creatorNeal-Sturgess, C. E.
dc.date2008-10-13
dc.date.accessioned2026-07-07T10:09:36Z
dc.date.available2026-07-07T10:09:36Z
dc.descriptionIt is the purpose of this short paper to show that the well known Griffiths theory of brittle fracture can be re-interpreted as a simple case of a modified Hamiltonian, and corresponds to a stationary action solution using the Euler-Lagrange equations. In this derivation it is still necessary to employ the equivalence with Irwins stress intensity factor approach to obtain the Griffith-Irwin equation. It is then shown that if physics of fracture is modelled using a simplified crack tip stress wave unloading model, then the Griffith-Irwin relationship can be derived in a single process, which is a major simplification of the procedure. Also the simplified crack tip stress wave unloading model employed gives a much clearer view of the basic physics of fracture. Keywords: Fracture, Griffiths, Hamiltonians, stress waves.
dc.description8 pages, 4 figures
dc.identifierhttps://arxiv.org/abs/0810.2218
dc.identifierhttp://arxiv.org/abs/0810.2218
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/171370
dc.subjectMaterials Science
dc.titleA Direct Derivation of the Griffith-Irwin Relationship using a Crack tip Unloading Stress Wave Model
dc.typetext

Files

Collections