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Investigating the Influence of the Electrochemical Environment on the Flotation of Bornite and Chalcocite

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Beneficiation of sulphide ores by flotation is ascribed to the natural electrochemical activity associated with sulphide minerals. Flotation is an electrochemical process comprising many interdependent conditions that are difficult to decouple in terms of controlling flotation performance. The extent of electrochemical activity is mineral dependent and can be measured against a reference cell to differentiate between minerals. This difference in activity is known as the rest potential. The rest potential can be exploited to preferentially float one mineral over another as these properties result in different regions of flotation stability for different minerals. Bornite and chalcocite present an interesting study because when measured against the standard hydrogen electrode (SHE), there is a small difference in rest potential; bornite has a potential of 0.44 V and chalcocite a potential of 0.40 V. The key differentiating factor between the two minerals is the presence of iron in bornite (Cu5FeS4) and the lack thereof in chalcocite (Cu2S). This study considers bornite and chalcocite microflotation, adsorption studies and zeta potential measurements, and three key factors were explored: pH, galvanic interactions and collector adsorption. The overall objective of the study is to understand the response of bornite and chalcocite to changes in pulp chemistry.
Title: Investigating the Influence of the Electrochemical Environment on the Flotation of Bornite and Chalcocite
Description:
Beneficiation of sulphide ores by flotation is ascribed to the natural electrochemical activity associated with sulphide minerals.
Flotation is an electrochemical process comprising many interdependent conditions that are difficult to decouple in terms of controlling flotation performance.
The extent of electrochemical activity is mineral dependent and can be measured against a reference cell to differentiate between minerals.
This difference in activity is known as the rest potential.
The rest potential can be exploited to preferentially float one mineral over another as these properties result in different regions of flotation stability for different minerals.
Bornite and chalcocite present an interesting study because when measured against the standard hydrogen electrode (SHE), there is a small difference in rest potential; bornite has a potential of 0.
44 V and chalcocite a potential of 0.
40 V.
The key differentiating factor between the two minerals is the presence of iron in bornite (Cu5FeS4) and the lack thereof in chalcocite (Cu2S).
This study considers bornite and chalcocite microflotation, adsorption studies and zeta potential measurements, and three key factors were explored: pH, galvanic interactions and collector adsorption.
The overall objective of the study is to understand the response of bornite and chalcocite to changes in pulp chemistry.

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