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Title: Brittle to ductile transition to cleavage fracture: Progress report, April 1-November 30, 1987

Technical Report ·
OSTI ID:5532281

The brittle-to-ductile transition in cleavage fracture in single crystals is being studied both experimentally and theoretically as the key problem in such fracture transitions exhibited by intrinsically brittle (cleavable) polycrystalline solids. The intrinsic process that governs the transition is thermally assisted dislocation emission from the tips of atomically sharp cleavage cracks at the verge of propagation, which then provide effective crack tip shielding and blunting. All other phenomena known to influence the transition in fracture, such as shielding provided through the polarization of free dislocations in the distant field, micro-crack initiation, etc., are identified as extrinsic processes that merely shift the basic transition to lower temperatures or higher crack velocities, or consider formation of cracks with the required velocity for cleavage propagation.

Research Organization:
Massachusetts Inst. of Tech., Cambridge (USA). Dept. of Mechanical Engineering
DOE Contract Number:
FG02-87ER45294
OSTI ID:
5532281
Report Number(s):
DOE/ER/45294-T1; ON: DE88004074
Resource Relation:
Other Information: Portions of this document are illegible in microfiche products
Country of Publication:
United States
Language:
English