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      Mercury mobility and bioavailability in soil from contaminated area

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          Interactions between mercury and dissolved organic matter--a review.

          Dissolved organic matter (DOM) interacts very strongly with mercury, affecting its speciation, solubility, mobility, and toxicity in the aquatic environment. Strong binding of mercury by DOM is attributed to coordination of mercury at reduced sulfur sites within the organic matter, which are present at concentrations much higher than mercury concentrations found in most natural waters. The ability of organic matter to enhance the dissolution and inhibit the precipitation of mercuric sulfide, a highly insoluble solid, suggests that DOM competes with sulfide for mercury binding. This is confirmed by very high conditional stability constants for mercury-organic sulfur (RSHg+) complexes (10(25)-10(32)) recently reported in literature. DOM appears to play a key role in the photochemical reduction of ionic mercury to elemental mercury and subsequent reoxidation of elemental mercury to ionic mercury, thus affecting volatilization loss and bioavailability of mercury to organisms. DOM affects the production and bioaccumulation of methylmercury, the most bioaccumulative mercury species in fish.
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            Selective extractions to assess the biogeochemically relevant fractionation of inorganic mercury in sediments and soils

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              X-ray Absorption Spectroscopic Evidence for the Complexation of Hg(II) by Reduced Sulfur in Soil Humic Substances

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                Author and article information

                Journal
                Environmental Geology
                Environ Geol
                Springer Nature
                0943-0105
                1432-0495
                September 2008
                October 11 2007
                : 55
                : 5
                : 1075-1087
                Article
                10.1007/s00254-007-1056-4
                acb85f2f-f4cd-41fb-bb96-12773f1ab192
                © 2007
                History

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