National Research Program, U.S. Geological Survey , 3215 Marine Street, Boulder, Colorado 80303, United States.
National Research Program, U.S. Geological Survey , 431 National Center, Reston, Virginia 20192, United States.
Environ Sci Technol. 2015 Oct 20;49(20):12169-77. doi: 10.1021/acs.est.5b02488. Epub 2015 Oct 1.
Anaerobic ammonium oxidation (anammox) couples the oxidation of ammonium with the reduction of nitrite, producing N2. The presence and activity of anammox bacteria in groundwater were investigated at multiple locations in an aquifer variably affected by a large, wastewater-derived contaminant plume. Anammox bacteria were detected at all locations tested using 16S rRNA gene sequencing and quantification of hydrazine oxidoreductase (hzo) gene transcripts. Anammox and denitrification activities were quantified by in situ (15)NO2(-) tracer tests along anoxic flow paths in areas of varying ammonium, nitrate, and organic carbon abundances. Rates of denitrification and anammox were determined by quantifying changes in (28)N2, (29)N2, (30)N2, (15)NO3(-), (15)NO2(-), and (15)NH4(+) with groundwater travel time. Anammox was present and active in all areas tested, including where ammonium and dissolved organic carbon concentrations were low, but decreased in proportion to denitrification when acetate was added to increase available electron supply. Anammox contributed 39-90% of potential N2 production in this aquifer, with rates on the order of 10 nmol N2-N L(-1) day(-1). Although rates of both anammox and denitrification during the tracer tests were low, they were sufficient to reduce inorganic nitrogen concentrations substantially during the overall groundwater residence times in the aquifer. These results demonstrate that anammox activity in groundwater can rival that of denitrification and may need to be considered when assessing nitrogen mass transport and permanent loss of fixed nitrogen in aquifers.
厌氧氨氧化(anammox)将氨的氧化与亚硝酸盐的还原偶联起来,产生氮气。在一个受大型废水污染物羽流影响的含水层的多个地点,研究了地下水厌氧氨氧化菌的存在和活性。使用 16S rRNA 基因测序和肼氧化还原酶(hzo)基因转录本定量检测,在所有测试地点均检测到厌氧氨氧化菌。通过在缺氧流路径中进行原位(15)NO2(-)示踪试验,在铵、硝酸盐和有机碳丰度不同的区域量化了厌氧氨氧化和反硝化活性。通过定量(28)N2、(29)N2、(30)N2、(15)NO3(-)、(15)NO2(-)和(15)NH4(+)随地下水运移时间的变化来确定反硝化和厌氧氨氧化的速率。在所有测试的区域都存在和活跃的厌氧氨氧化,包括当铵和溶解有机碳浓度较低时,但当添加乙酸以增加可用电子供应时,与反硝化相比,其比例下降。在该含水层中,厌氧氨氧化贡献了 39-90%的潜在 N2 产生,其速率约为 10 nmol N2-N L(-1) day(-1)。尽管示踪试验期间的厌氧氨氧化和反硝化速率都较低,但它们足以在含水层的整体地下水停留时间内大幅降低无机氮浓度。这些结果表明,地下水中的厌氧氨氧化活性可以与反硝化相媲美,在评估含水层中氮的质量输运和固定氮的永久损失时需要考虑到这一点。