The microstructural characteristics of ultra-high carbon hyper-eutectoid Fe
-C and Fe-C-Cu experimental steels have bern examined after isothermal tran
sformation in a range just beneath the eutectoid temperature. Particular at
tention was paid to the formation of so-called "abnormal ferrite", which re
fers to coarse ferrite grains which can form, in hyper-eutectoid compositio
ns, on the pro-eutectoid cementite before the pearlite reaction occurs. Thu
s it is confirmed that the abnormal ferrite is not a result of pearlite coa
rsening, hut of austenite decomposition before the conditions for coupled g
rowth of pearlite are established. The abnormal ferrite formed on both allo
triomorphic and Widmanstatten forms of pro-eutectoid cementite, and, signif
icantly, it was observed that the pro-eutectoid cementite continued to grow
, despite being enclosed by the abnormal ferrite. Under certain conditions
this could lead to the eventual formation of substantially reduced amounts
of pearlite. Thus, a model for carbon redistribution that allows the pro-eu
tectoid cementite to thicken concurrently with the abnormal ferrite is pres
ented. The orientation relationships between the abnormal ferrite and pro-e
utectoid cementite were also determined and found to be close to those whic
h have been reported between pearlitic ferrite and pearlitic cementite. (C)
2000 Ada Metallurgica Inc. Published by Elsevier Science Ltd. All rights r
eserved.