We report on a systematic analysis of x-ray photoelectron spectroscopy (XPS
) core- and valence-level spectra of clean and well-characterized iron oxid
e films, i.e., alpha-Fe2O3, gamma-Fe2O3, Fe3-deltaO4, and Fe3O4. All iron o
xide films were prepared epitaxially by NO2-assisted molecular-beam epitaxy
on single crystalline MgO(100) and alpha-Al2O3(0001) substrates. The phase
and stoichiometry of the films were controlled precisely by adjusting the
NO2 pressure during growth. The XPS spectrum of each oxide clearly showed s
atellite structures. These satellite structures were simulated using a clus
ter-model calculation, which could well reproduce the observed structures b
y considering the systematic changes in both the Fe 3d to O 2p hybridizatio
n and the d-d electron-correlation energy. The small difference in the sate
llite structures between alpha-Fe2O3 and gamma-Fe2O3 resulted mainly from c
hanges in the Fe-O hybridization parameters, suggesting an increased covale
ncy in gamma-Fe2O3 compared to alpha-Fe2O3. With increasing reduction in th
e gamma-Fe2O3-Fe3O4 system,the satellite structures in XPS became unresolve
d. This was not only due to the formation of Fe2+ ions, but also to nonhomo
geneous changes in the hybridization parameters between octahedral and tetr
ahedral Fe3+ ions. [S0163-1829(99)02704-6].