Grey and white cast irons were surface remelted using a high power CO2 lase
r with a scanning velocity in the range 0.5-200 mm s(-1) and the resulting
surface structures were investigated using optical microscopy and X-ray dif
fraction. The remelted surface of the white iron was composed of austenite
dendrites, which decompose to pearlite at low cooling rates and martensite
at medium cooling rates. The maximum volume fraction of martensite was obta
ined at 10 mm s(-1). The lattice parameter of the austenite increased with
increasing solidification velocity owing to solute trapping of carbon. The
remelted surface of the grey iron was composed of cellular ledeburite and X
-ray diffraction analyses of the grey specimen indicated the presence of au
stenite, martensite, graphite, cementite and epsilon phases. The initial au
stenite partially transformed to martensite at high cooling rates and to ep
silon phase at low cooling rates. The appearance of the epsilon phase is th
erefore linked to the decomposition of supersaturated austenite.