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Nitrate removal in a restored riparian groundwater system: functioning and importance of individual riparian zones

机译:恢复的河岸地下水系统中的硝酸盐去除:单个河岸区的功能和重要性

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For the design and the assessment of river restoration projects, it isimportant to know to what extent the elimination of reactive nitrogen (N) canbe improved in the riparian groundwater. We investigated the effectiveness ofdifferent riparian zones, characterized by a riparian vegetation succession,for nitrate (NO3−) removal from infiltrating river water in arestored and a still channelized section of the river Thur, Switzerland.Functional genes of denitrification (nirS and nosZ) wererelatively abundant in groundwater from willow bush and mixed forestdominated zones, where oxygen concentrations remained low compared to themain channel and other riparian zones. After flood events, a substantialdecline in NO3− concentration (> 50%) was observed in thewillow bush zone but not in the other riparian zones closer to the river. Inaddition, the characteristic enrichment of 15N and 18O in theresidual NO3− pool (by up to 22‰ for δ15N and upto 12‰ for δ18O) provides qualitative evidence that thewillow bush and forest zones were sites of active denitrification and, to alesser extent, NO3− removal by plant uptake. Particularly in thewillow bush zone during a period of water table elevation after a floodingevent, substantial input of organic carbon into the groundwater occurred,thereby fostering post-flood denitrification activity that reducedNO3− concentration with a rate of ~21 μmol N l?1 d?1. Nitrogen removal in the forestzone was not sensitive to flood pulses, and overall NO3− removalrates were lower (~6 μmol l?1 d−1). Hence,discharge-modulated vegetation–soil–groundwater coupling was found to be akey driver for riparian NO3− removal. We estimated that, despitehigher rates in the fairly constrained willow bush hot spot, totalNO3− removal from the groundwater is lower than in the extendedforest area. Overall, the aquifer in the restored section was more effectiveand removed ~20% more NO3− than the channelized section.
机译:对于河流修复项目的设计和评估,重要的是要知道在河岸地下水中可将活性氮(N)的消除程度提高多少。我们调查了以河岸植被演替为特征的不同河岸带对从河床中渗入的河水中存储的硝酸盐(NO 3 -)去除的效果,该河床仍是沟渠状的。来自瑞士柳树和森林混合带的地下水中反硝化作用的功能基因(nirS 和 nosZ )相对丰富,与主要通道和主要通道相比,这些区域的氧气浓度仍然较低其他河岸带。洪水事件发生后,在柳树灌木丛地区观察到NO 3 -浓度大幅下降(> 50%),而在其他靠近河流的河岸地区则没有。此外,残留NO 3 -池中 15 N和 18 O的特征富集(最多22) δ 15 N的‰和δ 18 O的高达12‰)提供了定性证据,表明柳树灌木丛和森林区是活跃反硝化的场所,在较小程度上,NO <通过植物吸收去除sub> 3 -。特别是在洪水事件发生后地下水位升高期间的柳树灌木丛地区,发生了向地下水中大量有机碳的输入,从而促进了洪水后的反硝化活性,从而降低了NO 3 - d ?1 。林区的氮去除对洪水脉冲不敏感,总的NO 3 -去除率较低(〜6μmoll ?1 d < sup> -1 )。因此,排放调节的植被-土壤-地下水的耦合被发现是河岸NO 3 -去除的关键驱动力。我们估计,尽管在相当受限制的柳灌木丛热点地区的比率较高,但从地下水中去除的总NO 3 -却比扩展森林地区的要低。总体而言,恢复部分中的含水层比通道化部分更有效,去除的NO 3 -约多20%。

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