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Trace metal mobility under varying redox conditions: modeling Cd and Zn release

机译:在不同氧化还原条件下的痕量金属迁移率:模拟镉和锌的释放

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Metal-contaminated riparian soils can be a source of metal release to surface water. The effects of varying redox conditions on mobility of zinc (Zn) and cadmium (Cd) were measured and modeled. Soil sampled from a riparian Spodosol contaminated with Cd and Zn was incubated in the laboratory under water-saturated conditions. The experiment was performed in a 3×3 factorial design with C-source (plant residue, 2 levels and control) and N amendments (NO3, NH4+, and control) as factors. Carbon was added to accelerate the rate of reducing the redox potential. We postulate that the mobility of Cd and Zn is critically affected by the change in pH, DOC, reductive dissolution of Fe(III) oxides and, potentially, sulphide precipitation on the long term The currently available data only reflect incipient reducing conditions (Eh not below 336 mV) and show hardly any change in soluble Cd and Zn that results from the counteracting effects of increasing soil pH, increasing DOC, and increasing Fe2+ that compete with Cd2+ and Zn2+ sorption. Speciation calculations (WHAM VI) confirm these trends.
机译:被金属污染的河岸土壤可能是金属释放到地表水中的来源。测量和模拟了不同氧化还原条件对锌(Zn)和镉(Cd)迁移率的影响。从被镉和锌污染的河岸坡藻中取样的土壤在实验室中在水饱和条件下进行培养。该实验以3×3因子设计进行,其中C源(植物残渣,2个水平和对照)和N个修饰物(NO3,NH4 +和对照)为因子。添加碳以加速降低氧化还原电势的速率。我们推测,镉和锌的迁移率受pH,DOC,Fe(III)氧化物的还原溶解以及长期可能硫化物沉淀的变化的影响很大。目前可获得的数据仅反映了初始还原条件(低于336 mV),几乎没有显示出可溶性Cd和Zn的任何变化,这是由于土壤pH升高,DOC增加以及Fe2 +与Cd2 +和Zn2 +吸附竞争而产生的。形态计算(WHAM VI)证实了这些趋势。

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