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- W2038996000 abstract "Sulfate enriched in 32S with respect to co-existent sulfur is found in the Orgeuil meteorite. Similar isotopic distributions can be effected with at least three laboratory procedures: (1) oxidation of FeS by traces of a strong oxidizing agent such as O2 or HOOH in a generally reducing aqueous environment, (2) bacterial oxidation of sulfides, or (3) reaction of elemental sulfur with water followed by partial oxidation of the unequilibrated products. For many reasons, the first mechanism is attractive for explaining the 32S/34S distribution in the carbonaceous chondrites." @default.
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- W2038996000 title "Isotopic composition of sulfur and sulfate produced by oxidation of FeS" @default.
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