X-ray photoelectron spectroscopy (XPS) is used in the present study to
investigate the oxidation state and the structural role of titanium i
n two melanites with different TiO2 content (similar to 3 % and simila
r to 6 % wt) from M.Vulture (Italy). The Ti2p-XPS spectra can be satis
factorily fitted when Ti3+ is lodged on octahedral and Ti4+ distribute
d over octahedral and tetrahedral sites. The XPS direct estimates of T
i site populations match very well with those indirectly obtained from
Mossbauer spectroscopy (MS) through the Fe distribution. In addition,
good agreement between the Fe2+/Fe3+ ratios estimated by both XPS and
MS has been found using Fe3O4 as a standard for interpreting Fe(2)p p
hotoelectron spectra.