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Physiological and molecular characterization of a microbial community established in unsaturated, petroleum-contaminated soil

机译:在非饱和,石油污染土壤中建立的微生物群落的生理和分子特征

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The microbial communities established in soil samples from an unsaturated, petroleum-contaminated zone and from an adjacent uncontaminated site were characterized by physiological and molecular approaches. Possible electron acceptors such as sulfate and nitrate had been completely depleted in these soil samples. Slurries of these soil samples were incubated in bottles in the presence of hydrocarbon indicators (benzene, toluene, xylene and decane), and the degradation of these compounds was examined. Supplementation with electron acceptors stimulated hydrocarbon degradation, although the stimulatory effect was small in the contaminated soil. The initial degradation rates in the contaminated soil under fermentative/methanogenic conditions were comparable to those under aerobic conditions. The microbial populations in the original soil samples were analysed by cloning and sequencing of polymerase chain reaction (PCR)-amplified bacterial and archaeal 16S rRNA gene fragments, showing that the sequences retrieved from these soils were substantially different. For instance, Epsilonproteobacteria, Gammaproteobacteria, Crenarchaeota and Methanosarcinales could only be detected at significant levels in the contaminated soil. Denaturing gradient gel electrophoresis (DGGE) analyses of 16S rRNA gene fragments amplified by PCR from the incubated soil-slurry samples showed that supplementation of the electron acceptors resulted in a shift in the major populations, while the DGGE profiles after incubating the contaminated soil under the fermentative/methanogenic conditions were not substantially changed. These results suggest that petroleum contamination of the unsaturated zone resulted in the establishment of a fermentative/methanogenic community with substantial hydrocarbon-degrading potential.
机译:通过生理和分子方法表征了来自不饱和,石油污染区和邻近未污染地点的土壤样品中建立的微生物群落。这些土壤样品中可能的电子受体(例如硫酸盐和硝酸盐)已被完全耗尽。将这些土壤样品的浆液在存在碳氢化合物指示剂(苯,甲苯,二甲苯和癸烷)的情况下在瓶中孵育,并检查这些化合物的降解情况。尽管受污染的土壤中的刺激作用很小,但添加电子受体会刺激碳氢化合物的降解。在发酵/产甲烷条件下,受污染土壤的初始降解速率与有氧条件下的降解速率相当。通过克隆和测序聚合酶链反应(PCR)扩增的细菌和古细菌16S rRNA基因片段,对原始土壤样品中的微生物种群进行了分析,显示从这些土壤中检索到的序列存在很大差异。例如,在受污染的土壤中仅能检测到大量的Epsilon变形杆菌,γ变形杆菌,Crenarchaeota和Methanosarcinales。通过PCR扩增的16S rRNA基因片段的变性梯度凝胶电泳(DGGE)分析从孵育的土壤浆液样品中显示,电子受体的添加导致主要种群的转移,而DGGE在孵育被污染的土壤下的DGGE谱后发酵/产甲烷的条件没有实质性改变。这些结果表明,不饱和区的石油污染导致建立了具有大量烃降解潜能的发酵/产甲烷群落。

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