A SUS308 stainless steel weldment of which main phases are ferrite and aust
enite was aged at 450 degrees C for a time period up to 11000 h in order to
investigate the compositional evolution of the ferrite by Mossbauer spectr
oscopy. Changes in the internal magnetic held of Fe with aging time suggest
that the ferrite decomposes by spinodal process finally to produce the Fe-
rich alpha and the Cr-rich alpha' phase. According to the mean internal mag
netic field measurement, the Cr content of the former is about 9 at% Cr whi
ch is consistent with a calculated phase diagram. The Cr content of the a'
phase is evaluated to be about 83 at% Cr by the isomer shift measurement, w
hich shows a slight deviation from the calculated phase diagram. The phase
decomposition is accompanied by an increase in the hardness of ferrite, whi
le that of austenite is remained unchanged.