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The surface chemistry of chalcopyrite during electrochemical dissolution Ghahremaninezhad Gharelar, Ahmad
Abstract
Hydrometallurgy may be an alternative to the currently practiced smelting process for copper extraction from chalcopyrite (CuFeS₂). However, the low temperature hydrometallurgical processes for chalcopyrite continue to face challenges, mostly relating to their slow dissolution rates or high sulfuric acid production. The slow dissolution rate of the mineral is strongly linked to the formation of the passive film on its surface. However, despite 40 years of research on this topic, there is still not a complete agreement between researchers about the composition and stability of chalcopyrite’s passive film in sulfuric acid solutions. In this work, the nature of chalcopyrite’s passive film and its stability were studied by application of a variety of electrochemical techniques. Additionally, the electrochemical results of the chalcopyrite study were compared to those obtained for a pyrrhotite electrode (Fe₁₋xS), as pyrrhotite electrochemistry represents a simplified case of the chalcopyrite system. X-ray photoelectron spectroscopy (XPS) was used to analyze the composition of the product layers formed on the surface. It is shown that the chalcopyrite electrode is passive for potentials up to 0.90 VSHE. Above this potential, transpassive dissolution occurs. Results of XPS studies have suggested that a metal-deficient sulfide film (Cu₁₋xFe₁₋yS₂₋z) is the most plausible copper and iron containing sulfide phase which passivates the surface of chalcopyrite. In addition, an outer layer of iron oxyhydroxide (FeOOH) forms on the passive film. FeOOH forms via oxidation of the passive film’s ferrous sulfide phases. The thickness of the sulfide passive film was calculated to be approximately 6.7 nm. 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 VSHE.
Item Metadata
Title |
The surface chemistry of chalcopyrite during electrochemical dissolution
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Creator | |
Publisher |
University of British Columbia
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Date Issued |
2012
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Description |
Hydrometallurgy may be an alternative to the currently practiced smelting process for
copper extraction from chalcopyrite (CuFeS₂). However, the low temperature
hydrometallurgical processes for chalcopyrite continue to face challenges, mostly relating to
their slow dissolution rates or high sulfuric acid production. The slow dissolution rate of the
mineral is strongly linked to the formation of the passive film on its surface. However,
despite 40 years of research on this topic, there is still not a complete agreement between
researchers about the composition and stability of chalcopyrite’s passive film in sulfuric acid
solutions. In this work, the nature of chalcopyrite’s passive film and its stability were studied
by application of a variety of electrochemical techniques. Additionally, the electrochemical
results of the chalcopyrite study were compared to those obtained for a pyrrhotite electrode
(Fe₁₋xS), as pyrrhotite electrochemistry represents a simplified case of the chalcopyrite
system. X-ray photoelectron spectroscopy (XPS) was used to analyze the composition of the
product layers formed on the surface.
It is shown that the chalcopyrite electrode is passive for potentials up to 0.90 VSHE.
Above this potential, transpassive dissolution occurs. Results of XPS studies have suggested
that a metal-deficient sulfide film (Cu₁₋xFe₁₋yS₂₋z) is the most plausible copper and iron
containing sulfide phase which passivates the surface of chalcopyrite. In addition, an outer
layer of iron oxyhydroxide (FeOOH) forms on the passive film. FeOOH forms via oxidation
of the passive film’s ferrous sulfide phases. The thickness of the sulfide passive film was
calculated to be approximately 6.7 nm. 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
VSHE.
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Genre | |
Type | |
Language |
eng
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Date Available |
2012-07-27
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Provider |
Vancouver : University of British Columbia Library
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Rights |
Attribution 3.0 Unported
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DOI |
10.14288/1.0072933
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URI | |
Degree | |
Program | |
Affiliation | |
Degree Grantor |
University of British Columbia
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Graduation Date |
2012-11
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Campus | |
Scholarly Level |
Graduate
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Rights URI | |
Aggregated Source Repository |
DSpace
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Item Media
Item Citations and Data
Rights
Attribution 3.0 Unported