The effects of heterogeneity and anisotropy on the size effect in cracked polycrystalline films

Citation
R. Ballarini et al., The effects of heterogeneity and anisotropy on the size effect in cracked polycrystalline films, INT J FRACT, 95(1-4), 1999, pp. 19-39
Citations number
20
Categorie Soggetti
Mechanical Engineering
Journal title
INTERNATIONAL JOURNAL OF FRACTURE
ISSN journal
03769429 → ACNP
Volume
95
Issue
1-4
Year of publication
1999
Pages
19 - 39
Database
ISI
SICI code
0376-9429(1999)95:1-4<19:TEOHAA>2.0.ZU;2-W
Abstract
A model is developed for quantifying the size effect due to heterogeneity a nd anisotropy in polycrystalline films. The Monte Carlo finite element calc ulations predict the average and standard deviation of the microscopic (loc al) stress intensity factors and energy release rate of a crack in a column ar aggregate of randomly orientated, perfectly bonded, orthotropic crystals (grains) under plane deformation. The boundary of the near-tip region is s ubjected to displacement boundary conditions associated with a macroscopic (far field or nominal) Mode-I stress intensity factor and average elastic c onstants calculated for the uncracked film with a large number of grains. T he average and standard deviation of the microscopic stress intensity facto rs and energy release rate, normalized with respect to the macroscopic para meters, are presented as functions of the number of grains within the near- tip region, and the parameters that quantify the level of crystalline aniso tropy. It is shown that for a given level of anisotropy, as long as the cra ck tip is surrounded by at least ten grains, then the expected value and st andard deviation of the crack tip parameters are insensitive to the number of crystals. For selected values of crystalline anisotropy, the probability distributions of Mode-I stress intensity factor and stress ahead of the cr ack are also presented. The results suggest that the size effect due to het erogeneity and anisotropy is weak; crack initiation load and direction are governed only by the details of the grains in the immediate vicinity of the crack tip.