“…When determining bulk properties from NEXAFS spectra by monitoring the fluorescence yield (FY), the presence of oxidised species at the surface is less important because of the several hundred nm analysis depth for FY. Todd et al (2003b) tacitly assumed that covellite contained both Cu(I) and Cu(II), but they did not provide an explanation for the apparent absence of evidence for Cu(II) in the Cu 2p photoelectron spectra for unoxidised covellite and chalcopyrite (e.g., Folmer and Jellinek, 1980;Buckley and Woods, 1984;Gebhardt et al, 1986). Also, mackinawite, the Fe(II) reference sulfide studied by Todd et al (2003b), is known to be unstable in air (Boursiquot et al, 2001).…”