Miller Daniel N, Smith Richard L
U.S. Geological Survey, 3215 Marine Street, Boulder, Colorado 80303, United States.
J Contam Hydrol. 2009 Jan 26;103(3-4):182-93. doi: 10.1016/j.jconhyd.2008.10.011. Epub 2008 Nov 5.
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 O2 (>300 microM) and NH4+ (51-800 microM). 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 O2, NH4+, and NO3- (0-300, 0-500, and 100-200 microM 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, NH4+ zone at the down-gradient site. Only a single Nitrosospira sequence was detected beneath the infiltration bed. Furthermore, the majority of Nitrosospira-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.
地下水硝化作用是一个特征描述较少的过程,它影响着氮的形态和迁移。利用针对硝化过程的基于培养和分子技术,对污染羽流中两个地点的岩芯进行了检测。第一个地点位于污水渗滤床下方,接收含有氧气(>300微摩尔)和铵离子(51 - 800微摩尔)的处理后废水。第二个地点在污染羽流中铵带前沿下游2.5公里处,具有氧气、铵离子和硝酸根离子的垂直梯度(随深度分别为0 - 300、0 - 500和100 - 200微摩尔)。通过基于培养的MPN方法计数的氨氧化菌和亚硝酸盐氧化菌在两个地点的丰度都很低(分别为1.8至350个/克和33至35000个/克)。在实验室对岩芯材料测量的潜在硝化活性也非常低,产物积累需要数周时间。对含水层DNA的分子分析(巢式PCR,随后进行克隆和16S rDNA测序)在下游地点的整个岩芯中主要检测到与亚硝化螺菌属相关的序列,在下游地点较深的缺氧铵带中检测到较小比例的亚硝化单胞菌属序列。在渗滤床下方仅检测到一个亚硝化螺菌序列。此外,大多数与亚硝化螺菌相关的序列代表一个未被识别的簇。我们得出结论,在地球化学稳定的下游地点,与亚硝化螺菌相关的一个未被表征的群体占主导地位,但在地球化学条件更易变的渗滤床下方,几乎没有发现β-变形菌硝化菌的证据。