真菌代谢物在低pH下稳定铀(VI):在环境生物技术中的应用

A. Ogar , A. Grandin , V. Sjöberg , K. Turnau , S. Karlsson
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引用次数: 12

摘要

土壤和水的铀污染是一个世界性的问题,由于地质或人为释放,如采矿,或使用无机肥料。由于铀的复杂化学性质,低污染和中度污染场地的原位修复是一个复杂的过程。该研究表明,在pH为3.5时,从未加工的含铀页岩中分离出的真菌菌株创造了水化学条件,可以在0.20 μm孔隙系统中固定97%的10 mg L-1溶解铀。重新分配在10分钟内发生,持续了5周,生物量中只有12%的库存被回收。溶相的粒径排除色谱法鉴定出的有机物的范围在60 kD到100 D之间,这是对孵育时间的响应。地球化学模拟表明铀-有机配合物的形成,其中配体的大小、配位化学和它们的聚集倾向决定了再分配。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Stabilization of Uranium(VI) at Low pH by Fungal Metabolites: Applications in Environmental Biotechnology

Uranium contamination of soils and water is a worldwide problem due to geology or anthropogenic release such as mining, or use of inorganic fertilizers. In situ remediation of low and moderately contaminated sites is a complicated procedure due to the complex chemistry of uranium. This study demonstrates that at pH 3.5, a fungal strain isolated from unprocessed uranium bearing shale creates hydrochemical conditions that immobilize 97% of a total of 10 mg L-1 dissolved uranium in a 0.20 μm pore system. The redistribution occurred within 10 minutes and remained for five weeks and just 12% of the inventory was retrieved in the biomass. Size exclusion chromatography of the dissolved phase identified organic substances in the range of more than 60 kD down to 100 D as a response to time of incubation. Geochemical modeling indicates formation of uranium-organic complexes where ligand size, coordination chemistry and their tendency to agglomerate determine the redistribution.

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