Center for Multiphase Environmental Research, Department of Chemical Engineering, Washington State University, Pullman, USA.
Biotechnol Bioeng. 2011 Feb;108(2):264-76. doi: 10.1002/bit.22956.
Removal of hexavalent uranium (U(VI)) from aqueous solution was studied using a Gram-positive facultative anaerobe, Cellulomonas sp. strain ES6, under anaerobic, non-growth conditions in bicarbonate and PIPES buffers. Inorganic phosphate was released by cells during the experiments providing ligands for formation of insoluble U(VI) phosphates. Phosphate release was most probably the result of anaerobic hydrolysis of intracellular polyphosphates accumulated by ES6 during aerobic growth. Microbial reduction of U(VI) to U(IV) was also observed. However, the relative magnitudes of U(VI) removal by abiotic (phosphate-based) precipitation and microbial reduction depended on the buffer chemistry. In bicarbonate buffer, X-ray absorption fine structure (XAFS) spectroscopy showed that U in the solid phase was present primarily as a non-uraninite U(IV) phase, whereas in PIPES buffer, U precipitates consisted primarily of U(VI)-phosphate. In both bicarbonate and PIPES buffer, net release of cellular phosphate was measured to be lower than that observed in U-free controls suggesting simultaneous precipitation of U and PO₄³⁻. In PIPES, U(VI) phosphates formed a significant portion of U precipitates and mass balance estimates of U and P along with XAFS data corroborate this hypothesis. High-resolution transmission electron microscopy (HR-TEM) and energy dispersive X-ray spectroscopy (EDS) of samples from PIPES treatments indeed showed both extracellular and intracellular accumulation of U solids with nanometer sized lath structures that contained U and P. In bicarbonate, however, more phosphate was removed than required to stoichiometrically balance the U(VI)/U(IV) fraction determined by XAFS, suggesting that U(IV) precipitated together with phosphate in this system. When anthraquinone-2,6-disulfonate (AQDS), a known electron shuttle, was added to the experimental reactors, the dominant removal mechanism in both buffers was reduction to a non-uraninite U(IV) phase. Uranium immobilization by abiotic precipitation or microbial reduction has been extensively reported; however, the present work suggests that strain ES6 can remove U(VI) from solution simultaneously through precipitation with phosphate ligands and microbial reduction, depending on the environmental conditions. Cellulomonadaceae are environmentally relevant subsurface bacteria and here, for the first time, the presence of multiple U immobilization mechanisms within one organism is reported using Cellulomonas sp. strain ES6.
采用革兰氏阳性兼性厌氧菌纤维素单胞菌(Cellulomonas sp. strain ES6),在碳酸氢盐和 PIPES 缓冲液中,于厌氧、非生长条件下,研究了从水溶液中去除六价铀(U(VI))。实验过程中细胞释放无机磷酸盐,为形成不溶性 U(VI)磷酸盐提供配体。磷酸盐的释放很可能是 ES6 在好氧生长过程中积累的细胞内多磷酸盐进行厌氧水解的结果。还观察到 U(VI)被微生物还原为 U(IV)。然而,生物(基于磷酸盐)沉淀和微生物还原去除 U(VI)的相对幅度取决于缓冲液化学性质。在碳酸氢盐缓冲液中,X 射线吸收精细结构(XAFS)光谱表明,固相中的 U 主要以非晶质铀(IV)相存在,而在 PIPES 缓冲液中,U 沉淀物主要由 U(VI)-磷酸盐组成。在碳酸氢盐和 PIPES 缓冲液中,测量到细胞磷酸盐的净释放量均低于无 U 对照,表明 U 和 PO₄³⁻同时沉淀。在 PIPES 中,U(VI)磷酸盐形成了 U 沉淀物的重要部分,U 和 P 的质量平衡估算以及 XAFS 数据证实了这一假设。PIPES 处理样品的高分辨率透射电子显微镜(HR-TEM)和能量色散 X 射线光谱(EDS)确实显示了 U 固体的细胞外和细胞内积累,纳米级的薄片结构包含 U 和 P。然而,在碳酸氢盐中,去除的磷酸盐量超过了根据 XAFS 确定的 U(VI)/U(IV)分数所需的化学计量平衡,这表明在该系统中 U(IV)与磷酸盐一起沉淀。当蒽醌-2,6-二磺酸盐(AQDS),一种已知的电子穿梭体,添加到实验反应器中时,两种缓冲液中的主要去除机制都是还原为非晶质铀(IV)相。通过生物沉淀或微生物还原来固定铀已有广泛报道;然而,目前的工作表明,根据环境条件,菌株 ES6 可以通过与磷酸盐配体沉淀和微生物还原同时从溶液中去除 U(VI)。纤维素单胞菌科是环境相关的地下细菌,这是首次在一种细菌中发现 Cellulomonas sp. strain ES6 具有多种 U 固定机制。