首页> 外文期刊>Geoderma: An International Journal of Soil Science >Controlled variation of redox conditions in a floodplain soil: impact on metal mobilization and biomethylation of arsenic and antimony.
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Controlled variation of redox conditions in a floodplain soil: impact on metal mobilization and biomethylation of arsenic and antimony.

机译:洪泛区土壤中氧化还原条件的受控变化:对金属迁移以及砷和锑的生物甲基化的影响。

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摘要

An automated biogeochemical microcosm system allowing the control of redox potential (EH) in soil suspensions was used to assess the effect of EH on the mobility of cadmium (Cd), copper (Cu), nickel (Ni), zinc (Zn), iron (Fe), and manganese (Mn) as well as on the methylation of arsenic (As) and antimony (Sb) in a contaminated and slightly acidic floodplain soil. The experiment was conducted under stepwise variation from reducing (approximately -300 mV at pH 5) to oxidizing (+600 mV at pH 5) conditions. The EH was found to be an important factor controlling the dynamics of studied compounds and elements. Concentrations of Cd, Cu, Mn, Ni, and Zn in solution were low at low EH and increased with rising EH what might be attributed to the interaction with dissolved organic carbon (DOC), Mn, and precipitation as sulphides. Redox potential and pH correlate significantly with Cd, Ni, Cu, Zn, and Mn. Total Fe concentrations in solution were high at low EH and dropped sharply at EHi) and antimony (Sbi), momomethyl arsenic (MMAs), monomethyl antimony (MMSb), and dimethyl arsenic (DMAs) in solution decreased significantly with rising EH, indicating that low EH promotes the mobility of these compounds.
机译:利用能够控制土壤悬浮液中氧化还原电位(E H )的自动化生物地球化学缩影系统,评估E H 对镉(Cd)迁移率的影响,铜(Cu),镍(Ni),锌(Zn),铁(Fe)和锰(Mn)以及砷和砷(Sb)在受污染且微酸性的洪泛区土壤中的甲基化作用。在从还原(pH值为5约为-300 mV)到氧化(pH 5值为+600 mV)的逐步变化下进行实验。发现E H 是控制所研究化合物和元素动力学的重要因素。在低E H 下溶液中Cd,Cu,Mn,Ni和Zn的浓度较低,并且随着E H 的升高而增加,这可能是由于与溶解有机物的相互作用碳(DOC),锰和硫化物沉淀。氧化还原电势和pH与Cd,Ni,Cu,Zn和Mn显着相关。溶液中的总Fe浓度在低E H 时较高,而在pH <5的E H i )和锑(Sb i ),甲基甲基砷(MMA),一甲基锑(MMSb)和二甲基砷(DMA)的浓度降低随E H 的增加而显着增加,表明低E H 促进了这些化合物的迁移。

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