G. Spanos et Mg. Hall, THE FORMATION MECHANISM(S), MORPHOLOGY, AND CRYSTALLOGRAPHY OF FERRITE SIDEPLATES, Metallurgical and materials transactions. A, Physical metallurgy andmaterials science, 27(6), 1996, pp. 1519-1534
The formation mechanism(s), morphology, and crystallography of seconda
ry ferrite sideplates were investigated with transmission electron mic
roscopy (TEM), scanning electron microscopy (SEM), electron backscatte
r pattern (EBSP) analysis, and optical microscopy in a high-purity Fe-
0.12 wt pet C-3.3 wt pet Ni alloy isothermally transformed at temperat
ures of 550 degrees C, 600 degrees C, 650 degrees C, and 675 degrees C
. The results indicate that two different mechanisms contribute to the
formation of these sideplates at austenite grain boundaries. On the f
irst mechanism, primary sideplates form initially, followed by rapid l
ateral impingement along their bases, resulting in a region along the
grain boundary which very early in the growth process resembles an all
otriomorphic film. On the second mechanism, sympathetic nucleation of
ferrite sideplates occurs atop pre-existing ferrite allotriomorphs, re
sulting in ferrite:ferrite grain boundaries and significant crystallog
raphic misorientations between the sideplates and the allotriomorphs w
ith which they are associated. These results indicate that ''secondary
sideplates'' and the allotriomorphs from which they evolve are not co
mposed of monolithic single crystals formed by a morphological instabi
lity mechanism but are instead composed of multiple crystals formed by
individual nucleation events. Previous investigations in Ti-Cr alloys
and a high chromium stainless steel suggest that the findings present
ed here may be applicable to a number of other alloy systems as well.