An austenitic Fe-25Cr-19Ni stainless steel alloy was carbonitrided at 1,000
degrees C in an atmosphere with a(c) = 1 and P(N-2)=0.9atm to form two dis
crete precipitation zones. Local equilibrium between the precipitates and t
he austenite matrix carbon activity was achieved throughout the reaction zo
ne. Small, globular Cr7C3 particles were formed immediately beneath the sur
face. High aspect ratio Cr23C6 lamellar plates were formed deeper in the pr
ecipitation zone and were found to have a cube-cube orientation relationshi
p with the austenite matrix. The inward growth of these carbides was facili
tated by the formation of an austenite/depleted austenite grain boundary at
the precipitation front, which transformed the austenite to a more appropr
iate orientation and accelerated the segregation of chromium to the carbide
tips.