“…Two weak cathodic maxima at approximately 0.15 and À0.25 V, and a current surge at potentials more negative than À0.3 V are observed on the negative-going sweep; the charge associated with the reduction is much less than that passed in the electrooxidation processes. Similar data have previously been acquired at different arsenopyrite electrodes (Kostina and Chernyak, 1976;Cruz et al, 1997;Lázaro et al, 1997;Lin and Zheng, 1997;Costa et al, 2002); they are consistent with the idea that a passivating layer decomposes at high enough overpotentials, thereby accelerating the oxidation of underlying mineral. In the second cycle, the surges of cathodic and anodic currents are shifted to more negative and more positive potentials, respectively, extending the passivity region; the cathodic maximum arising at about +0.4 V is due to the reduction of Fe(III) species.…”