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Intergranular fracture by slip/grain boundary interaction

Journal Article · · Metallurgical Transactions, A (Physical Metallurgy and Materials Science); (United States)
DOI:https://doi.org/10.1007/BF02646987· OSTI ID:6934779
 [1];  [2]
  1. Oak Ridge National Lab., TN (United States)
  2. State Univ. of New York, Stony Brook, NY (United States). Dept. of Materials Science and Engineering
One of the outstanding problems in materials science is to explain why certain intermetallic compounds are inherently strong but notoriously weak at grain boundaries (GBs). The role of interaction between slip dislocations and [110] tilt boundaries in crack nucleation has been analyzed for the face-centered cubic (fcc) and L1[sub 2] structures. Dislocation absorption into the boundaries is orientation-dependent according to the elastic anisotropy. When the transfer of slip across the boundary is impeded, cleavage fracture is predicted on the (1[bar 1]1) plane. Intergranular fracture can be initiated when a symmetric double pileup of primary slip dislocations from both sides of the boundary occurs simultaneously. The available experimental data on slip/grain boundary interaction and intergranular fracture are in good agreement with the present predictions.
DOE Contract Number:
AC05-84OR21400
OSTI ID:
6934779
Journal Information:
Metallurgical Transactions, A (Physical Metallurgy and Materials Science); (United States), Journal Name: Metallurgical Transactions, A (Physical Metallurgy and Materials Science); (United States) Vol. 21A; ISSN 0360-2133; ISSN MTTABN
Country of Publication:
United States
Language:
English