A Vibrational Spectroscopic O-18 Tracer Study Of Pyrite Oxidation

Pergamon-elsevier Science Ltd
Publication Type:
Journal Article
Geochimica Et Cosmochimica Acta, 1991, 55 (6), pp. 1609 - 1614
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Pyrite was oxidised under O-18(2) gas in H-2 O-16 solutions, with and without added ferric ion, and the sulfate produced was analysed by vibrational spectroscopy to determine the relative amounts of sulfate isotopomers ((SOnO4-n2-)-O-16-O-18) formed. At
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