Synthetic iron oxides (goethite, alpha-FeO . OH; hematite, Fe2O3; and
ferrihydrite, Fe(OH)(3)) were used as model compounds to simulate the
mineralogy of surface films on carbon steel. Dissolution of these oxid
es exposed to pure cultures of the metal-reducing bacterium, Shewanell
a putrefaciens, was followed by direct atomic absorption spectroscopy
measurement of ferrous iron coupled with microscopic analyses using co
nfocal laser scanning and environmental scanning electron microscopies
. During an 8-day exposure the organism colonized mineral surfaces and
reduced solid ferric oxides to soluble ferrous ions. Elemental compos
ition, as monitored by energy dispersive x-ray spectroscopy, indicated
mineral replacement reactions with both ferrihydrite and goethite as
iron reduction occurred. When carbon steel electrodes were exposed to
S. putrefaciens, microbiologically influenced corrosion was demonstrat
ed electrochemically and microscopically.