Institute of Radiochemistry, Helmholtz Centre Dresden-Rossendorf, Dresden, Germany.
J Hazard Mater. 2011 Dec 15;197:1-10. doi: 10.1016/j.jhazmat.2011.09.049. Epub 2011 Oct 2.
This work describes the mechanisms of uranium biomineralization at acidic conditions by Bacillus sphaericus JG-7B and Sphingomonas sp. S15-S1 both recovered from extreme environments. The U-bacterial interaction experiments were performed at low pH values (2.0-4.5) where the uranium aqueous speciation is dominated by highly mobile uranyl ions. X-ray absorption spectroscopy (XAS) showed that the cells of the studied strains precipitated uranium at pH 3.0 and 4.5 as a uranium phosphate mineral phase belonging to the meta-autunite group. Transmission electron microscopic (TEM) analyses showed strain-specific localization of the uranium precipitates. In the case of B. sphaericus JG-7B, the U(VI) precipitate was bound to the cell wall. Whereas for Sphingomonas sp. S15-S1, the U(VI) precipitates were observed both on the cell surface and intracellularly. The observed U(VI) biomineralization was associated with the activity of indigenous acid phosphatase detected at these pH values in the absence of an organic phosphate substrate. The biomineralization of uranium was not observed at pH 2.0, and U(VI) formed complexes with organophosphate ligands from the cells. This study increases the number of bacterial strains that have been demonstrated to precipitate uranium phosphates at acidic conditions via the activity of acid phosphatase.
这项工作描述了在酸性条件下,球形芽孢杆菌 JG-7B 和鞘氨醇单胞菌 S15-S1 这两种从极端环境中回收的微生物将铀矿化的机制。U-细菌相互作用实验是在低 pH 值(2.0-4.5)下进行的,在这种条件下,铀的水相形态主要由高迁移性的铀酰离子组成。X 射线吸收光谱(XAS)表明,所研究的菌株在 pH 值为 3.0 和 4.5 时将铀沉淀为属于准钙铀云母族的磷酸铀矿物相。透射电子显微镜(TEM)分析表明,铀沉淀物在菌株之间具有特异性定位。对于球形芽孢杆菌 JG-7B,U(VI)沉淀物与细胞壁结合。然而,对于鞘氨醇单胞菌 S15-S1,U(VI)沉淀物既在细胞表面又在细胞内观察到。在没有有机磷酸盐底物的情况下,在这些 pH 值下检测到了土著酸性磷酸酶的活性,与观察到的 U(VI)生物矿化有关。在 pH 值为 2.0 时没有观察到铀的生物矿化,并且 U(VI)与来自细胞的有机磷酸配体形成配合物。这项研究增加了已经证明可以通过酸性磷酸酶的活性在酸性条件下沉淀铀磷酸盐的细菌菌株的数量。