Rust on weathering steels exposed for up to 11 y in industrial and rur
al environments exhibited a spotty, nonuniform appearance as a result
of contrast between light and dark areas on the surface. The area of t
he lighter regions Increased with exposure time, as well as with incre
asing alloy content Microscopic examination of cross sections revealed
the dark regions had a porous appearance. The lighter regions were si
milar except for the presence of a relatively thin, smooth outer-surfa
ce layer. Raman spectroscopy indicated the dark, porous rust was compr
ised of goethite and lepidocrocite, while the smooth outer layer on th
e light areas was composed of hematite (alpha-Fe2O3) and magnetite (Fe
3O4). Electrochemical potential measurements indicated the lighter are
as were more passive. Results suggested formation of the thin outer la
yer of alpha-Fe2O3 and Fe3O4 is an important part of the mechanism of
protective rust formation on weathering steels in the environments stu
died.