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Change in Bacterial Community Structure during In Situ Biostimulation of Subsurface Sediment Cocontaminated with Uranium and Nitrate

机译:铀和硝酸盐共污染的地下沉积物原位生物刺激过程中细菌群落结构的变化

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摘要

Previous studies have demonstrated that metal-reducing microorganisms can effectively promote the precipitation and removal of uranium from contaminated groundwater. Microbial communities were stimulated in the acidic subsurface by pH neutralization and addition of an electron donor to wells. In single-well push-pull tests at a number of treated sites, nitrate, Fe(III), and uranium were extensively reduced and electron donors (glucose, ethanol) were consumed. Examination of sediment chemistry in cores sampled immediately adjacent to treated wells 3.5 months after treatment revealed that sediment pH increased substantially (by 1 to 2 pH units) while nitrate was largely depleted. A large diversity of 16S rRNA gene sequences were retrieved from subsurface sediments, including species from the α, β, δ, and γ subdivisions of the class Proteobacteria, as well as low- and high-G+C gram-positive species. Following in situ biostimulation of microbial communities within contaminated sediments, sequences related to previously cultured metal-reducing δ-Proteobacteria increased from 5% to nearly 40% of the clone libraries. Quantitative PCR revealed that Geobacter-type 16S rRNA gene sequences increased in biostimulated sediments by 1 to 2 orders of magnitude at two of the four sites tested. Evidence from the quantitative PCR analysis corroborated information obtained from 16S rRNA gene clone libraries, indicating that members of the δ-Proteobacteria subdivision, including Anaeromyxobacter dehalogenans-related and Geobacter-related sequences, are important metal-reducing organisms in acidic subsurface sediments. This study provides the first cultivation-independent analysis of the change in metal-reducing microbial communities in subsurface sediments during an in situ bioremediation experiment.
机译:先前的研究表明,还原金属的微生物可以有效地促进铀的沉淀和从受污染的地下水中去除铀。通过pH中和和向孔中添加电子供体,可刺激酸性地下微生物的群落。在多个处理位置的单井推挽试验中,硝酸盐,Fe(III)和铀被大量还原,电子供体(葡萄糖,乙醇)被消耗。在处理后3.5个月对紧邻处理井的岩心中进行的沉积物化学检查表明,沉积物的pH值显着增加(增加了1至2个pH单位),而硝酸盐却被大量消耗。从地下沉积物中检索到多种多样的16S rRNA基因序列,包括变形杆菌属α,β,δ和γ细分的物种,以及低和高G + C革兰氏阳性物种。在对被污染的沉积物中的微生物群落进行原位生物刺激后,与先前培养的还原金属的δ-变形杆菌相关的序列从克隆文库的5%增加到了近40%。定量PCR显示,在四个受测位点中的两个位点,经生物刺激的沉积物中的Geobacter型16S rRNA基因序列增加了1-2个数量级。定量PCR分析的证据证实了从16S rRNA基因克隆文库中获得的信息,表明δ-变形杆菌科的成员(包括脱氧厌氧杆菌相关和地杆菌相关的序列)是酸性地下沉积物中重要的金属还原生物。这项研究为原位生物修复实验中地下沉积物中还原金属的微生物群落变化提供了首次独立于栽培的分析。

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