Surface Oxidation of Pyrite as a Function of pH

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Abstract

Pyrite, the most abundant metal sulfide at the surface of Earth, plays a key role in many processes such as acid mine drainage, redox cycling of metals at oxic-anoxic boundaries of lake bottom, and degradation of pollutants. The oxidation of pyrite was studied in batch experiments over a large range of pH (2.5−12), with trace oxygen. Surface analysis of the samples was performed using X-ray photoelectron spectroscopy (XPS). Speciation of the aqueous species was investigated by inductively coupled plasma atomic emission spectrometry (ICP-AES), ionic chromatography, and UV−vis spectrophotometry. The pyrite surface can drastically change with the pH, which was never at steady state and tended to reach an acidic value whatever the initial pH. For pH <4, Fe(II) and SO42- were released into solution; from XPS analyses, the pyrite surface presented O−H groups, an Fe-deficient composition Fe1-xS2, and iron(III) (hydr)oxide traces. Whatever the pH, the sulfur of the FeS2 surface was mainly under the (−I) state oxidation. When the pH increased, Fe(II) disappeared and the surface was covered with iron(III) (hydr)oxides. This overlayer did not passivate the sample against further oxidation, and a decrease in pH was still observed.

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