Electrochemical and XPS analysis of chalcopyrite (CuFeS2) dissolution in sulfuric acid solution

被引:267
|
作者
Ghahremaninezhad, A. [1 ]
Dixon, D. G. [1 ]
Asselin, E. [1 ]
机构
[1] Univ British Columbia, Dept Mat Engn, Vancouver, BC V6T 1Z4, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Mineral; Chalcopyrite; Electrochemical dissolution; Passivation; X-RAY PHOTOELECTRON; SURFACE OXIDATION; HINDERED DISSOLUTION; ANODIC-DISSOLUTION; ALKALINE-SOLUTIONS; PYRITE SURFACES; FERRIC ION; SPECTROSCOPY; SULFIDE; COPPER;
D O I
10.1016/j.electacta.2012.07.119
中图分类号
O646 [电化学、电解、磁化学];
学科分类号
081704 ;
摘要
The influence of potential on the species and surface films formed during electrodissolution of chalcopyrite were investigated in 0.5 M sulfuric acid solution at 25 degrees C. Cyclic voltammetry, chronoamperometry, potentiostatic and potentiodynamic polarization methods were applied. X-ray diffraction (XRD) and X-ray photoelectron spectroscopy (XPS) were used to analyze the minerals and product layers on the surface before and after electrodissolution. The chalcopyrite electrode was shown to be passive for potentials up to 0.90 V-SHE. Above this potential, transpassive dissolution occurs. Results of XPS studies have suggested that a metal-deficient sulfide film (Cu1-xFe1-yS2-z) consisting of cuprous sulfide (Cu-S) and iron sulfide (Fe-S) bonds, is the most plausible copper and iron containing sulfide phase which passivates the surface of chalcopyrite. It is demonstrated that the transpassive dissolution of chalcopyrite is significantly linked to oxidation of sulfur (from sulfide in the passive film to elemental sulfur and maybe sulfur species with higher oxidation states, e.g. thiosulfate). No elemental sulfur or polysulfide species were detected on the surface for potentials below 0.90 V-SHE. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:97 / 112
页数:16
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