“…In principle, the study of the Fe L 2,3 -edge XAS spectra in Fe oxides may provide information about the oxidation state and, in some cases, allow one to separate the contributions of the magnetic moments of Fe ions in tetrahedral and octahedral sites (van Aken & Liebscher, 2002;van der Laan & Kirkman, 1992;Crocombette et al, 1995). More recently, Fe L 2,3 -edge XMCD has also been at the centre of many of the characterization studies of nominal magnetite NPs (Park et al, 2004;Goering et al, 2006;Huang et al, 2004;Yamasaki et al, 2009). However, the most common iron oxides exhibit similar Fe L 2,3 XAS and XMCD spectra because they are mainly governed by the point symmetry at the absorbing site (octahedral and tetrahedral in this case).…”