“…Aside from elemental sulfur, thiosulfate, sulfate, various compounds of As in oxidation states up to +5, and Fe(III)-O species were found on arsenopyrite reacted under various conditions by XPS Walker, 1988-1989;Richardson and Vaughan, 1989;Nesbitt et al, 1995;Schaufuss et al, 2000;Costa et al, 2002;Jones et al, 2003;Mikhlin et al, 2003b), Raman spectroscopy (McGuire et al, 2001b,c;Costa et al, 2002), and X-ray absorption spectroscopy (XANES) (Mikhlin and Tomashevich, 2005). Several researchers Walker, 1988-1989;Nesbitt et al, 1995;Costa et al, 2002;Mikhlin et al, 2003a,b) pointed out the formation of nonstoichiometric, S-rich surface layers which were considered responsible for passivity of mineral sulfides (Buckley et al, 1985;Hackl et al, 1995;Mikhlin et al, 2003aMikhlin et al, , 2004a.…”