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Spectroscopic and microscopic characterization of uranium biomineralization in Myxococcus xanthus

机译:葡萄球菌中铀生物矿化的光谱学和微观表征

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In this work, synchrotron-based X-ray absorption spectroscopy (XAS) and transmission electron microscopy (TEM) studies were carried out to elucidate at molecular scale the interaction mechanisms of Myxococcus xanthus with uranium at different pH values. Extended X-ray absorption fine structure (EXAFS) spectroscopic measurements showed that there are significant differences in the structural parameters of the U complexes formed by this bacterium at pH 2 and 4.5. At very low acidic pH of 2, the cells accumulated U( VI) as organic phosphate-metal complexes. At pH 4.5, however, the cells of this bacterium precipitated U( VI) as meta-autunitelike phase. TEM analyses demonstrated that at pH 2 the uranium accumulates were located mainly at the cell surface, whereas at pH 4.5 a uranium precipitation occurred on the cell wall and within the extracellular polysaccharides (EPS) characteristic of this bacterium. Dead/live staining studies showed that 30% and 50% of the uranium treated cell populations were alive at pH 2 and 4.5, respectively. The precipitation of U(VI) as mineral meta-autunitelike phase is possibly due to the bacterial acidic phosphatase activity. The precipitation of uranium as mineral phases may lead to more stable U(VI) sequestration that may be suitable for remediation purposes. These observations, combined with the very high uranium accumulation capability of the studied bacterial cells indicate that M. xanthus may significantly influence the fate of uranium in soil environments where these bacterial species are mainly found.
机译:在这项工作中,进行了基于同步加速器的X射线吸收光谱(XAS)和透射电子显微镜(TEM)研究,以阐明在不同pH值下,黄色葡萄球菌与铀的相互作用机理。扩展的X射线吸收精细结构(EXAFS)光谱测量表明,在pH 2和4.5时,这种细菌形成的U复合物的结构参数存在显着差异。在2的非常低的酸性pH值下,细胞以有机磷酸盐-金属配合物形式积累U(VI)。然而,在pH 4.5下,该细菌的细胞沉淀出U(VI),为亚金铁矿样相。 TEM分析表明,在pH值为2时,铀积累主要位于细胞表面,而在pH值为4.5时,铀沉淀出现在细胞壁上以及该细菌特有的细胞外多糖(EPS)中。死/活染色研究表明,铀处理的细胞群中30%和50%分别在pH 2和4.5下存活。 U(VI)沉淀为矿物亚铁矿样相可能是由于细菌酸性磷酸酶活性所致。铀作为矿物相的沉淀可能导致更稳定的U(VI)螯合,可能适用于修复目的。这些观察结果与所研究细菌细胞的极高铀积累能力相结合,表明黄腐分支杆菌可能在主要发现这些细菌物种的土壤环境中显着影响铀的命运。

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