In this investigation, the methodology, advantages, and limitations of usin
g Orientation Imaging Microscopy (OIM) to study microstructures in multipha
se steels are examined. In particular, proeutectoid ferrite precipitation h
as been investigated in a hypoeutectoid steel (Fe-0.12%C-3%Ni), while the p
roeutectoid cementite transformation has been studied in a hypereutectoid s
teel (Fe-1.3%C-13%Mn). By utilizing misorientation maps and inverse pole fi
gure maps to determine the orientation differences between individual cryst
als, the internal morphology of the solid-state precipitates has been deter
mined. What appear by other types of imaging to be monolithic single crysta
ls are shown to be aggregates of finer crystals with misorientations betwee
n them. The relative quality of the Electron Backscatter Diffraction (EBSD)
patterns has been correlated to specific phases and to interphase and grai
n boundaries using pattern quality maps (also referred to as image quality
maps). These techniques have been adapted for quantitative identification o
f different microconstituents, including volume fraction measurements. By m
aking comparisons among optical micrographs, conventional SEM micrographs,
pattern quality maps, inverse pole figure maps, and misorientation maps, th
e advantages and limitations of different types of OIM mapping for studying
different aspects of phase transformations in steels are elucidated. (C) 2
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