Abstract
Conditions for the formation of a nonequilibrium nonstoichiometric metal-deficient layer (NL) on natural pyrrhotites are studied, together with the NL electroreduction and the role NL plays in a nonoxidizing dissolution of pyrrhotite in solutions of sulfuric and hydrochloric acids. To estimate the NL weight, the charge connected with a cathodic peak at about –0.2 V (Ag/AgCl) is used. The peak reflects the irreversible reduction of NL with the formation of hydrogen sulfide, which is confirmed by SEM and XES data. Bulky NL forms in 0.5 M H2SO4at –0.1 to 0.0 V, where the nonoxidizing dissolution rate sharply alters, and at 0.5–1.1 V, where the pyrrhotite oxidation rate is high. The NL growth is controlled by solid-state diffusion, whereas nonoxidizing dissolution of iron is limited by diffusion at 20–30°C and a kinetic stage of dissolution of sulfur at higher temperatures.
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Kuklinskii, A.V., Mikhlin, Y.L., Pashkov, G.L. et al. Conditions for the Formation of a Nonequilibrium Nonstoichiometric Layer on Pyrrhotite in Acid Solutions. Russian Journal of Electrochemistry 37, 1269–1276 (2001). https://doi.org/10.1023/A:1013231612008
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DOI: https://doi.org/10.1023/A:1013231612008