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- W1502169660 abstract "We quantified the in4situ rates of dissimilatory SO4 24 4reduction and the resulting S biomineralisation products in an acid4sulfate soil landscape which had been re4flooded by controlled tidal inundation. SO 4 24 4 reduction was confined to the near4surface, formerly4drained soil layers and occurred at rates up to ~300 nmol/cm 3 /day. Elemental S was the dominant short4term product of SO 4 24 4reduction, and was present at up ~40 9mol S/g. It was generally more abundant than iron4monosulfides or iron4disulfides in recently re4flooded soil layers. However, as expected, iron4disulfides were increasingly significant in soil layers that had experienced long4term inundation (i.e. 40480 9molS/g formed over ~5 years)." @default.
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- W1502169660 date "2010-01-01" @default.
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- W1502169660 title "Reductive sulfur biomineralisation in a re-flooded acid-sulfate soil landscape." @default.
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