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Journal ArticleDOI

Evidence for microbiological manganese oxidation in the river Tamar Estuary, South West England

TLDR
Water samples from the Tamar Estuary oxidized manganese when supplemented with Mn 2+ (2 mgl −1 ). The rates of oxidation were depressed in the presence of various metabolic inhibitors as discussed by the authors.
Abstract
Water samples from the Tamar Estuary oxidized manganese when supplemented with Mn 2+ (2 mgl −1 ). The rates of oxidation were depressed in the presence of various metabolic inhibitors. The effect of Mn 2+ and temperature on the rate of manganese oxidation suggested that a biological process was largely responsible for converting Mn 2+ to Mn 4+ . Rates of manganese oxidation were much higher in freshwater (3·32 μgl −1 h −1 in water containing 30 mgl −1 of suspended matter) than in saline water (0·7 μgl −1 h −1 in water of salinity 32‰) containing the same amount of particulate matter. The rate of manganese oxidation was proportional to the particulate load (up to 100 mgl −1 particulates).

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Effect of sunlight on redox cycles of manganese in the southwestern Sargasso Sea

TL;DR: In this paper, the authors investigated the cycling of manganese between soluble Mn(II) and particulate oxides in the upper 750 m at a station in the southwestern Sargasso Sea.
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Photoreduction of manganese oxides in seawater

TL;DR: Sunlight increased the dissolution rate of synthetic oxides in seawater, an effect that increased with the duration of light exposure as mentioned in this paper, and showed an even larger stimulatory effect on the reductive dissolution of natural oxides.
Journal ArticleDOI

Microbial oxidation of manganese in a North Carolina estuary

TL;DR: In this article, the formation of manganese oxides in seawater from the lower Newport River estuary, North Carolina, was investigated and it was shown that the formation was due to the microbially catalyzed oxidation of Mn(I) to Mn(II) oxides (MnO).
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Role of sediment resuspension in the remobilization of particulate-phase metals from coastal sediments.

TL;DR: Results indicate that sediment resuspension is a very important mechanism for releasing metals into the water column and provide new insight into the chemical and physical processes controlling the long-term fate of trace metals in contaminated sediments.
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The fate of trace metals in suspended matter in a mangrove creek during a tidal cycle

TL;DR: In this paper, the variation of heavy metal content in suspended matter (SM) during tidal cycles in a mangrove creek was described, and the stable isotope of carbon was used as a tracer for sources of SM to the system.
References
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Journal ArticleDOI

The surface chemistry of hydrous manganese dioxide

TL;DR: An experimental investigation has shown that H+ and OH− are potential determining ions for the δMnO2 surface The pH (ZPC) was determined using electrophoretic mobilities and Na+ and K+ adsorption and found to be 225 Alkalimetric titration curves failed to provide a direct determination of the pH as mentioned in this paper.
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Environmental oxidation rate of manganese(II): bacterial catalysis

TL;DR: A simple mass balance for dissolved manganese (II) in waters containing low levels of oxygen in Saanich Inlet indicates that the residence time for Mn(II) removal to the solid phase is on the order of a few days as discussed by the authors.
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Recent trends in research on heavy-metal contamination in the sea

TL;DR: In this article, a review of recent trends in the study of metal contamination in the sea is presented, which includes the input of metals to the sea and their deposition in the sediments, the influence of environmental and biological factors on the accumulation of metals by the biota and the use of organisms as indicators of contamination.
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Pathways of manganese in an open estuarine system

TL;DR: The distribution of Mn was examined in the bottom sediments and water column (suspended paniculate matter) of the Laurentian Trough as mentioned in this paper, and a characteristic profile of Mn with depth in the sediment consisted of a Mn-enriched surface oxidized zone, less than 20 mm thick, and a Mndepleted subsurface reducing zone.
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