During a XPS study of oxide growth and segregation on commercial alumi
nium-silicon alloys, problems were encountered in the application of C
1s charge referencing. Using the C1s peak maximum as a reference, shif
ts were observed in the aluminium and magnesium peak positions, partic
ularly after high temperature oxidation, which could not be accounted
for. Referencing against the native oxide O1s peak corrected the shift
s. A consequent analysis of the C1s spectra revealed that the hydrocar
bon contamination was reacting under the conditions used to oxidise th
e alloys. From the XPS results it is deduced that active sites on the
oxidised alloy surface are responsible for catalytic cracking and oxid
ation of the adventitious hydrocarbon. Parallel studies on other heat
treated oxidic systems have produced similar results. It is recommende
d that an alternative to C1s charge referencing should be used when pe
rforming XPS studies on heat treated oxidic systems.