Unified analysis of phase-field models for cohesive fracture

Fuente: arXiv
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Autore principale: Wu, Jian-Ying
Natura: Preprint
Pubblicazione: 2024
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author Wu, Jian-Ying
author_facet Wu, Jian-Ying
contents We address in this review unified analysis of phase-field models for cohesive fracture. Aiming to regularize the Barenblatt (1959) cohesive zone model, all the discussed models are distinguished by three characteristic functions, i.e., the geometric function dictating the crack profile, the degradation function for the constitutive relation and the dissipation function defining the crack driving force. The latter two functions coincide in the associated formulation, while in the non-associated one they are designed to be different. Distinct from the counterpart for brittle fracture, in the phase-field model for cohesive fracture the regularization length parameter has to be properly incorporated into the dissipation and/or degradation functions such that the failure strength and traction-separation softening curve are both well-defined. Moreover, the resulting crack bandwidth needs to be non-decreasing during failure in order that imposition of the crack irreversibility condition does not affect the anticipated traction-separation law (TSL). With a truncated degradation function that is proportional to the length parameter, the Conti et al.(2016) model and the latter improved versions can deal with crack nucleation only in the vanishing limit and capture cohesive fracture only with a particular TSL. Owing to a length scale dependent degradation function of rational fraction, these deficiencies are largely overcome in the phase-field cohesive zone model (PF-CZM). Among many variants in the literature, only with the optimal geometric function, can the associated PF-CZM apply to general non-concave softening laws and the non-associated uPF-CZM to (almost) any arbitrary one. Some mis-interpretations are clarified and representative numerical examples are presented.
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id arxiv_https___arxiv_org_abs_2412_03836
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Unified analysis of phase-field models for cohesive fracture
Wu, Jian-Ying
Materials Science
We address in this review unified analysis of phase-field models for cohesive fracture. Aiming to regularize the Barenblatt (1959) cohesive zone model, all the discussed models are distinguished by three characteristic functions, i.e., the geometric function dictating the crack profile, the degradation function for the constitutive relation and the dissipation function defining the crack driving force. The latter two functions coincide in the associated formulation, while in the non-associated one they are designed to be different. Distinct from the counterpart for brittle fracture, in the phase-field model for cohesive fracture the regularization length parameter has to be properly incorporated into the dissipation and/or degradation functions such that the failure strength and traction-separation softening curve are both well-defined. Moreover, the resulting crack bandwidth needs to be non-decreasing during failure in order that imposition of the crack irreversibility condition does not affect the anticipated traction-separation law (TSL). With a truncated degradation function that is proportional to the length parameter, the Conti et al.(2016) model and the latter improved versions can deal with crack nucleation only in the vanishing limit and capture cohesive fracture only with a particular TSL. Owing to a length scale dependent degradation function of rational fraction, these deficiencies are largely overcome in the phase-field cohesive zone model (PF-CZM). Among many variants in the literature, only with the optimal geometric function, can the associated PF-CZM apply to general non-concave softening laws and the non-associated uPF-CZM to (almost) any arbitrary one. Some mis-interpretations are clarified and representative numerical examples are presented.
title Unified analysis of phase-field models for cohesive fracture
topic Materials Science
url https://arxiv.org/abs/2412.03836