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Precipitation of technetium by subsurface sulfate-reducing bacteria

机译:地下硫酸盐还原菌对of的沉淀

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To study the interaction between Tc and subsurface bacteria, we conducted batch experiments with soil and groundwater or sterilized deionized water. The system water/soil was amended with lactate and phosphate for bacterial growth. Nitrate and sulfate were added to stimulate the growth of indigenous denitrifying and sulfate-reducing bacteria. During denitrification Tc-concentration did not change with time. In the presence of sulfate-reducing bacteria, Tc-concentrations decreased in reacted waters which could be attributed to Tc(VII) reduction and precipitation of TcO2 and/or TcS2. Coprecipitation with newly formed iron sulfide is expected to contribute to Tc removal. Additional experiments with U and Tc showed that these elements were simultaneously reduced by sulfate-reducing bacteria. This work shows that 1) subsurface mixed cultures of denitrifying bacteria do not remove Tc from solution, this is different from uranium and 2) sulfate-reducing bacteria reduce and remove Tc from aqueous solutions and thus in situ bioremediation of subsurface waters and soils may be possible with such ubiquitous bacteria. [References: 20]
机译:为了研究Tc与地下细菌之间的相互作用,我们使用土壤和地下水或无菌去离子水进行了批量试验。用乳酸和磷酸盐对系统的水/土壤进行修正,以使细菌生长。加入硝酸盐和硫酸盐可刺激本地反硝化细菌和硫酸盐还原菌的生长。在反硝化过程中,Tc浓度不会随时间变化。在还原硫酸盐的细菌的存在下,反应水中的Tc浓度降低,这可能归因于Tc(VII)的还原以及TcO2和/或TcS2的沉淀。与新形成的硫化铁共沉淀有望有助于Tc的去除。用U和Tc进行的其他实验表明,这些元素被硫酸盐还原菌同时还原。这项工作表明,1)反硝化细菌的地下混合培养不会从溶液中去除Tc,这与铀不同; 2)还原硫酸盐的细菌会从水溶液中去除Tc,因此对地下水和土壤进行原位生物修复可能是可行的。这种无处不在的细菌是可能的。 [参考:20]

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