The formation of iron sulphide on oxidised pyrite during sulphidisation and subsequent interactions with xanthate

•Sulphidisation of oxidized pyrite at −200 mV (SHE) reduced the amount of ferric-hydroxide and generated elemental sulphur.•Sulphidisation of oxidized pyrite at −200 mV (SHE) could not convert the oxidised surface into an iron sulphide form.•Iron sulphide species were only formed on oxidised pyrite...

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Bibliographic Details
Published inMinerals engineering Vol. 157; p. 106564
Main Authors Huai, Yangyang, Peng, Yongjun
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.10.2020
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Summary:•Sulphidisation of oxidized pyrite at −200 mV (SHE) reduced the amount of ferric-hydroxide and generated elemental sulphur.•Sulphidisation of oxidized pyrite at −200 mV (SHE) could not convert the oxidised surface into an iron sulphide form.•Iron sulphide species were only formed on oxidised pyrite after the sulphidisation at a potential below −300 mV (SHE).•The newly sulphidised pyrite surface reacted with xanthate at a potential of 100 mV (SHE).•The newly formed iron sulphide species started to oxidise from a potential of −50 mV (SHE). Pyrite can be partially or completely oxidised during the stockpiling of pyritic ores, leading to a poor flotation performance. Sulphidisation with potential control has been commonly practised to convert the oxidised pyrite surface into a sulphide form before flotation. However, the lack of agreement on the suitable potential for the formation of iron sulphide species on the oxidised pyrite surface makes this practice genuinely uncertain. Using electrochemical techniques, this work identified that it was only at a potential below −300 mV that the sulphidisation with Na2S could generate iron sulphide species on the oxidised pyrite surface. In order to have the newly sulphidised pyrite surface to react with xanthate, the potential had to be elevated to 100 mV, but the newly formed iron sulphide species started to oxidise at a potential of around −50 mV. These findings provide a fundamental understanding of the nature of sulphidisation of oxidised sulphide minerals and a guideline to improve their flotation.
ISSN:0892-6875
1872-9444
DOI:10.1016/j.mineng.2020.106564