首页> 外文期刊>Journal of Contaminant Hydrology >Microbial Characterization Of Nitrification In A Shallow, Nitrogen-contaminated Aquifer, Cape Cod, Massachusetts And Detection Of A Novel Cluster Associated With Nitrifying Betaproteobacteria
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Microbial Characterization Of Nitrification In A Shallow, Nitrogen-contaminated Aquifer, Cape Cod, Massachusetts And Detection Of A Novel Cluster Associated With Nitrifying Betaproteobacteria

机译:浅层,氮污染的含水层,鳕鱼角,马萨诸塞州的硝化微生物特征以及与硝化β-变形杆菌相关的新型簇的检测

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Groundwater nitrification is a poorly characterized process affecting the speciation and transport of nitrogen. Cores from two sites in a plume of contamination were examined using culture-based and molecular techniques targeting nitrification processes. The first site, located beneath a sewage effluent infiltration bed, received treated effluent containing O_2 (>300 μM) and NH_4~+ (51 -800 μM). The second site was 2.5 km down-gradient near the leading edge of the ammonium zone within the contaminant plume and featured vertical gradients of O_2, NH_4~+, and NO_3~- (0-300, 0-500, and 100-200 μM with depth, respectively). Ammonia- and nitrite-oxidizers enumerated by the culture-based MPN method were low in abundance at both sites (1.8 to 350 g~(-1) and 33 to 35,000 g~(-1), respectively). Potential nitrifying activity measured in core material in the laboratory was also very low, requiring several weeks for products to accumulate. Molecular analysis of aquifer DNA (nested PCR followed by cloning and 16S rDNA sequencing) detected primarily sequences associated with the Nitrosospira genus throughout the cores at the down-gradient site and a smaller proportion from the Nitrosomonas genus in the deeper anoxic, NH_4~+ zone at the down-gradient site. Only a single Nitrosospira sequence was detected beneath the infiltration bed. Furthermore, the majority of Mitrosospira-associated sequences represent an unrecognized cluster. We conclude that an uncharacterized group associated with Nitrosospira dominate at the geochemically stable, down-gradient site, but found little evidence for Betaproteobacteria nitrifiers beneath the infiltration beds where geochemical conditions were more variable.
机译:地下水硝化是一个影响较广的过程,影响氮的形成和运输。使用针对硝化过程的基于培养物和分子技术,检查了污染羽流中两个位置的岩心。第一个站点位于污水流出物渗透床下方,接受了含有O_2(> 300μM)和NH_4〜+(51 -800μM)的处理后流出物。第二个位置是污染物羽流中铵带前沿附近的2.5 km向下梯度,并且具有O_2,NH_4〜+和NO_3〜-(0-300、0-500和100-200μM)的垂直梯度深度)。通过基于培养的MPN方法枚举的氨和亚硝酸氧化剂在两个位置的丰度都较低(分别为1.8至350 g〜(-1)和33至35,000 g〜(-1))。在实验室的核心材料中测得的潜在硝化活性也非常低,需要几周的时间才能积聚产品。含水层DNA的分子分析(巢式PCR,然后进行克隆和16S rDNA测序)主要检测到与下降梯度位点整个核心的亚硝基螺旋体属相关的序列,以及在较深的缺氧区NH_4〜+区中亚硝基孢属的比例较小在下降的站点。在渗透床下面仅检测到一个亚硝基螺旋菌序列。此外,大多数与拟螺旋体相关的序列代表了无法识别的簇。我们得出的结论是,与亚硝基螺菌有关的一个未知群体在地球化学稳定的下降梯度位点上占主导地位,但是在地球化学条件变化较大的渗透床下,没有发现β变形杆菌硝化器的证据。

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