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首页> 外文期刊>Geochemistry International >Biogenic Factors of Formation of Geochemical Uranium Anomalies near the Sludge Storage of the Novosibirsk Chemical Concentrate Plant
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Biogenic Factors of Formation of Geochemical Uranium Anomalies near the Sludge Storage of the Novosibirsk Chemical Concentrate Plant

机译:新西伯利亚化学浓缩植物污泥储存附近地球化学铀异常形成的生物学因素

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摘要

This paper presents evidence on the possible impact of aerobic and anaerobic microbiological processes on uranium migration in upper aquifers polluted by sulfates and nitrates at the Novosibirsk chemical concentrate plant (PAO NCCP). Uranium can be immobilized in local areas with high contents of organic substances, and the most important microbiological process is a decrease in redox potential owing to aerobic respiration, which can be followed under anaerobic conditions by redox-dependent uranium reduction in areas with negative Eh values. Moreover, in the presence of sufficient amounts of sulfate ions, further anaerobic processes of microbial sulfate and iron reduction result in the formation of iron sulfide, which serves as an antioxidant buffer in the case of oxygen infiltration into the sediment and transforms to molecular sulfur or sulfate preventing uranium oxidation.
机译:本文介绍了有氧和厌氧微生物过程可能影响的有氧和厌氧微生物过程对由硫酸盐和硝酸盐污染的上含水层中铀迁移的可能影响(Pao NCCP)。 铀可以固定在具有高含量的有机物质的局部区域,最重要的微生物过程是由于有氧呼吸的氧化还原电位的降低,可通过氧化氧依赖性铀的降低在厌氧条件下进行氧化氧化物条件 。 此外,在存在足够量的硫酸盐离子的情况下,进一步的微生物硫酸盐的厌氧过程和铁还原导致铁硫化铁的形成,其用作氧气浸润到沉积物中的抗氧化缓冲液并转化为分子硫或转化 硫酸盐预防铀氧化。

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