Manganese, iron and sulfur cycling in a coastal marine sediment, Aarhus bay, Denmark
The seasonal variation in oxidized and reduced pools of Mn, Fe and S, as well as the rates of SO 4 2− reduction, were studied in a fine-grained sediment. Below the 1–5 mm thick oxic zone, a zone of net Mn reduction extended to 1–2 cm depth, while iron reduction was found to 4–6 cm depth. Although th...
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Veröffentlicht in: | Geochimica et cosmochimica acta 1994-12, Vol.58 (23), p.5115-5129 |
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