PSI - Issue 66
Domenico Ammendolea et al. / Procedia Structural Integrity 66 (2024) 396–405 Author name / Structural Integrity Procedia 00 (2025) 000–000
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2. Theoretical Background This section provides the most important theoretical concepts at the base of the proposed modeling approach. In particular, an overview of the Cohesive Phase-Field Model proposed by Wu (Wu, 2017; Wu et al., 2020) is reported.
Fig. 1. Schematic representation of the smearing of an internal sharp crack.
Fig. 1 shows a two-dimensional domain u t and an internal sharp crack face c . Tractions t act on t , while the displacements u are imposed on u . Under these assumptions, the governing equations for structural mechanics, in the weak form, are: : d d d 0 C u u f u t u (1) where C is the isotropic elastic tensor, while u and f represent the virtual displacements and the body forces (per unit volume) vectors, respectively. In general, the PFM replaces the internal sharp crack face with a smeared interface by introducing a continuous scalar crack phase-field variable c , which evolves between 0 (intact material) and 1 (fully fractured material). In addition, the PFM defines a crack surface function c c , expresses in terms of c and its spatial gradient c , which, according to Wu formulation (Wu, 2017), is evaluated as follows: 2 R , which has an external discontinuous boundary
0 0 1 1 c l
c
(2)
, c c
l
0
c
c
In Eq. (2), 0 l is an internal length scale regularizing the cohesive sharp crack, 0 c represents a scaling parameter, and c is the crack geometric function describing how the material’s stiffness degrades as the crack evolves. The latter can be defined as: c 2 c c (1 ) 0 (3)
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