Y. Ohmori et al., Bainite transformation and the diffusional migration of bainite/austenite broad interfaces in Fe-9%Ni-C alloys, ACT MATER, 49(16), 2001, pp. 3149-3162
The processes of bainitic structure formation in Fe-9%Ni-C alloys have been
investigated by means of transmission electron and hot stage optical micro
scopies. The bainite laths formed initially with sharp surface reliefs grow
in thickness direction rather slowly with surface rumpling-type reliefs. A
pearlitic layer often forms in the carbon-enriched region between the bain
itic ferrite laths. The pearlitic ferrite nucleates epitaxially on or grows
directly from an adjacent bainitic ferrite lath. Such pearlite colonies al
ways exhibit the Isaichev ferrite/cementite orientation relationship with t
he [010](theta)parallel to < 111 > alpha parallel to < 110 > (gamma) near i
nvariant line between three phases on the bainite habit plane. In the typic
al upper bainite with cementite layer between ferrite laths, a cementite/fe
rrite orientation relationship with the (100)(theta)approximate to parallel
to {110}(alpha) bainite habit plane was recognised in addition to the (011
)(alpha)parallel to((1) over bar 03)(theta) habit. The general feature of c
ementite Precipitation in such upper bainite laths is that the near invaria
nt [010](theta)parallel to < 111 > (alpha)parallel to < 110 > (gamma), dire
ction lies on the bainite habit plane. (C) 2001 Acta Materialia Inc. Publis
hed by Elsevier Science Ltd. All rights reserved.