✍ Scribed by J. Païdassi; M.L. Pointud; R. Caillat; R. Darras
No coin nor oath required. For personal study only.
Fm. 3. Replica from a (100) fr8cture f8ce showing coherent precipitation in 8110~. x 7500
all able to form sessile dislocations resulting in a situation which is favourable for the operation of another slip system which will not form sessile dislocations. Friedel(s) has suggested that in a metal of high stacking fault energy, recombination of looked dislocations on octahedral planes could result in (100)
[llO] slip. The present, experiments show that not only is such slip easier as the temperature is raised, but also that it is most likely to occur in regions of substantial prior octahedral slip, e.g. in the vicinity of the fracture.
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