“…X-ray photoelectron spectroscopy data for CuFe 0.94 Ge 0.06 S 2 (Figure 4) reveals the presence of Cu + , Fe 3+ and S 2-, as has been observed in XPS data for unsubstituted chalcopyrites. 25,29,31,48,49 However, an additional weak peak (Figure 4b) corresponding to Fe 2+ is observed in the Fe 2p spectrum, suggesting that Ge substitution results in a reduction of a fraction of the Fe 3+ ions to Fe 2+ . A similar observation has been made for tin and indium substitution in chalcopyrite 30,31 Significantly, the 3d spectrum of Ge (Figure 4d) indicates that this cation is in a mixed oxidation state, with peaks assignable to both Ge 2+ and Ge 4+ present; the latter having the higher intensity.…”