Metallographic examination of archeological phosphoric iron and specially p
repared iron-phosphorus alloys sometimes reveals unusual 'ghosting' feature
s within ferrite grains when nital is used as an etch. The ghostlines mark
the boundaries in phosphorus content arising from the dual phase ferrite-au
stenite microstructure, which existed at elevated temperatures. Nital prefe
rentially attacks iron with lower phosphorus content, so giving a surface r
elief that characterises the phosphorus. Both ferrite-austenite and austeni
te-ferrite transformations occur by nucleation and growth, and also are acc
ompanied by the diffusion of phosphorus. The morphologies of phases formed
conform to the Dube classification system. The microstructures observed in
archeological irons are consistent with those produced by the ferrite-auste
nite transformation. Hence, understanding of the microstructures produced i
n this current work allows fuller interpretation of the microstructures fou
nd in archeological artefacts. MST/4404 (C) 2000 IoM Communications Ltd.