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- W2912490099 endingPage "354" @default.
- W2912490099 startingPage "345" @default.
- W2912490099 abstract "The mineral pyrite is considered the most common form of the sulfide minerals. Its oxidation is a very important process in nature, which involves in the redox recycling of iron. However, because of the growing need for the industrial production, sulfide oxidation produces more and more acid mine (or rock) drainage. This acid drainage has become a heavy economic and environmental problem. This review describes the oxidation mechanism of pyrite in an aqueous medium, including general oxidation and microbial oxidation, where sulfate, ferrous ion, S 0 , polysulfides, iron[III], and some intermediate species are formed. Also included is recent evidence on the electrochemical oxidation determined using the electrochemical method, X‐ray photoelectron spectroscopy (XPS), Raman spectroscopy, Fourier transform infrared spectroscopy (FTIR), and other techniques. In addition, the factors that influence the oxidation and dissolution rate, and the descriptive approaches for different species are discussed." @default.
- W2912490099 created "2019-02-21" @default.
- W2912490099 creator A5003060867 @default.
- W2912490099 creator A5010651513 @default.
- W2912490099 creator A5049555808 @default.
- W2912490099 creator A5058994392 @default.
- W2912490099 creator A5075480929 @default.
- W2912490099 date "2019-01-31" @default.
- W2912490099 modified "2023-10-16" @default.
- W2912490099 title "Pyrite oxidation mechanism in aqueous medium" @default.
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