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The Applications of Chemical Analyses of Sediments and Soils in ...

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operation. Wastewater is a major source <strong>of</strong> heavy metal contam<strong>in</strong>ation (Helz et al,1975). Rapid decrease <strong>in</strong> concentration <strong>of</strong> Zn, Cu, Pb, <strong>and</strong> Cd below the outfall <strong>in</strong>toBlack River, Maryl<strong>and</strong> was attributed to processes other than dilution, such asadsorption, precipitation, colloidal flocculation or biological uptake scaveng<strong>in</strong>g themetals from the water <strong>and</strong> deposit<strong>in</strong>g them <strong>in</strong> the sediments. Intense algae bloomswere noted with day time pH <strong>of</strong>ten above 9.0 compared with average effluent pH <strong>of</strong> 6.9lead<strong>in</strong>g to rapid deposition <strong>of</strong> trace metal hydroxides, carbonates or phosphates, <strong>and</strong>possibly <strong>in</strong>creased sorption on organic <strong>and</strong> <strong>in</strong>organic particles.Algae have also been found to concentrate heavy metals <strong>and</strong> as they die <strong>and</strong>s<strong>in</strong>k carry the heavy metals <strong>in</strong>to the sediments (Mart<strong>in</strong> <strong>and</strong> Knauer, 1973). Cadmiumappears to remobilize from the sediment possibly by cation exchange, or ag<strong>in</strong>g <strong>and</strong>decay <strong>of</strong> organic material, or solubilization as aqueous complexes (Helz et al, 1975).Acidity <strong>and</strong> colloid content, both <strong>in</strong>organic (clays) <strong>and</strong> organic (humic material),are important factors govern<strong>in</strong>g metal solubility, exchange <strong>and</strong> mobility.Total soluble metals <strong>in</strong> soil (<strong>and</strong> sediment) are made up <strong>of</strong> simple ions,hydrolysis species, complexes <strong>and</strong> chelated species (L<strong>in</strong>dsay, 1975). For metals withmore than one valence state, solubility <strong>and</strong> m<strong>in</strong>eral transformations are affected byredox state. Measurement <strong>of</strong> ion activities can be useful.Initial contact <strong>of</strong> water soluble metals with soil or sediment, particularly underbasic conditions, normally results <strong>in</strong> precipitation, first highly amorphous with large7

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