2018
DOI: 10.1002/pamm.201800157
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Restrictions in phase field modeling of brittle fracture

Abstract: A key feature of phase field approaches to fracture is the relatively simple structure of the method. However, current approaches inevitably exhibit some limitations which do not seem to be obvious and are therefore neglected in many investigations. The assumption of isotropic stiffness degradation by a scalar phase field parameter does not capture the anisotropy introduced by a crack and severely restricts the scope of application. Widely used tension-compression splits violate the specific conditions at crac… Show more

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Cited by 6 publications
(10 citation statements)
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“…Thus, such approaches generally violate crack boundary conditions and lead to a spurious phase field evolution [10]. Thus, the deviation of the approximated surface energy from the theoretical value becomes significant unless the crack is many times longer than ℓ, as illustrated in [12]. While the energy consumption of a smeared crack is approximated quite well for a small, but non-vanishing internal length ℓ the crack tip consumes additional energy which is not accounted for in the method [11].…”
Section: Critical Issues With Regard To Simulation Of Indentation Framentioning
confidence: 99%
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“…Thus, such approaches generally violate crack boundary conditions and lead to a spurious phase field evolution [10]. Thus, the deviation of the approximated surface energy from the theoretical value becomes significant unless the crack is many times longer than ℓ, as illustrated in [12]. While the energy consumption of a smeared crack is approximated quite well for a small, but non-vanishing internal length ℓ the crack tip consumes additional energy which is not accounted for in the method [11].…”
Section: Critical Issues With Regard To Simulation Of Indentation Framentioning
confidence: 99%
“…traction-free, it is feasible here to omit any split in the calculation of stress (1) and consider a full stiffness degradation (3) 1 . Referring to the discussion in [12], the degradation function g = (4 − a s ) S 3 + (a s − 3) S 4 of fourth-order with a s = 1 × 10 −4 is an optimal compromise to reduce the internal length sufficiently, but also guarantees that the phase field approaches the broken state. Since brittle materials tend to fail normal to the maximum principal stress, the phase field S should be driven by positive principal stresses rather than strains.…”
Section: Constitutive Choice Of Stiffness Degradation and Phase Fieldmentioning
confidence: 99%
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