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希瓦氏菌MR-1在流动式和间歇式反应器中对铀(VI)的去除比较

Comparison of uranium(VI) removal by Shewanella oneidensis MR-1 in flow and batch reactors.

作者信息

Sani Rajesh K, Peyton Brent M, Dohnalkova Alice

机构信息

Department of Chemical and Biological Engineering, South Dakota School of Mines and Technology, Rapid City, SD 57701, USA.

出版信息

Water Res. 2008 Jun;42(12):2993-3002. doi: 10.1016/j.watres.2008.04.003. Epub 2008 Apr 7.

Abstract

To better understand the interactions among metal contaminants, nutrients, and microorganisms in subsurface fracture-flow systems, biofilms of pure culture of Shewanella oneidensis MR-1 were grown in six fracture-flow reactors (FFRs) of different geometries. The spatial and temporal distribution of uranium and bacteria were examined using a tracer dye (brilliant blue FCF) and microscopy. The results showed that plugging by bacterial cells was dependent on the geometry of the reactor and that biofilms grown in FFRs had a limited U(VI)-reduction capacity. To quantify the U(VI)-reduction capacity of biofilms, batch experiments for U(VI) reduction were performed with repetitive U(VI) additions. U(VI)-reduction rates of stationary phase cultures decreased after each U(VI) addition. After the fourth U(VI) addition, stationary phase cultures treated with U(VI) with and without spent medium yielded gray and black precipitates, respectively. These gray and black U precipitates were analyzed using high-resolution transmission electron microscopy, energy-dispersive X-ray spectroscopy, and X-ray diffraction. Data for randomly selected areas of black precipitates showed that reduced U particles (3-6 nm) were crystalline, whereas gray precipitates were a mixture of crystalline and amorphous solids. Results obtained in this study, including a dramatic limitation of S. oneidensis MR-1 and its biofilms to reduce U(VI) and plugging of FFRs, suggest that alternative organisms should be targeted for stimulation for metal immobilization in subsurface fracture-flow systems.

摘要

为了更好地理解地下裂隙流系统中金属污染物、养分和微生物之间的相互作用,在六个不同几何形状的裂隙流反应器(FFR)中培养了嗜铁素还原地杆菌MR-1的纯培养生物膜。使用示踪染料(亮蓝FCF)和显微镜检查了铀和细菌的时空分布。结果表明,细菌细胞的堵塞取决于反应器的几何形状,并且在FFR中生长的生物膜具有有限的U(VI)还原能力。为了量化生物膜的U(VI)还原能力,进行了重复添加U(VI)的U(VI)还原批次实验。每次添加U(VI)后,固定相培养物的U(VI)还原率都会下降。在第四次添加U(VI)后,添加有和没有用过的培养基的U(VI)处理的固定相培养物分别产生了灰色和黑色沉淀。使用高分辨率透射电子显微镜、能量色散X射线光谱和X射线衍射对这些灰色和黑色的U沉淀进行了分析。黑色沉淀随机选择区域的数据表明,还原的U颗粒(3-6纳米)是结晶的,而灰色沉淀是结晶和无定形固体的混合物。本研究获得的结果,包括嗜铁素还原地杆菌MR-1及其生物膜在还原U(VI)方面的显著局限性以及FFR的堵塞,表明应针对替代生物进行刺激,以实现地下裂隙流系统中金属的固定。

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