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Abundance, Activity and Community Structure of Denitrifiers in Drainage Ditches in Relation to Sediment Characteristics, Vegetation and Land-Use

机译:与沉积物特征,植被和土地利用有关排水沟中脱氮机的丰富,活动和社区结构

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Drainage ditches are ubiquitous yet understudied features of the agricultural landscape. Nitrogen pollution disrupts the nutrient balance of drainage ditch ecosystems, as well as the waterbodies in which they drain. Denitrification can help ameliorate the impact of N-fertilization by converting reactive nitrogen into dinitrogen gas. However, factors affecting denitrification in drainage ditches are still poorly understood. In this study, we tested how within-ditch and regional environmental conditions affect denitrifier activity, abundance, and community structure, to understand controls on denitrification at multiple scales. To this end, we quantified in situ denitrification rates and denitrifier abundance in 13 drainage ditches characterized by different types of sediment, vegetation and land-use. We determined how denitrification rates relate to denitrifier abundance and community structure, using the presence of nirS, nirK and nosZ genes as a proxy. Denitrification rates varied widely between the ditches, ranging from 0.006 to 24 mmol N m(-2) h(-1). Ditches covered by duckweed, which contained high nitrate concentrations and had fine, sandy sediments, were denitrification hotspots. We found highest rates in ditches next to arable land, followed by those in grasslands; lowest rates were observed in peatlands and nature reserves. Denitrification correlated to nitrate concentrations, but not to nirK, nirS and nosZ abundance, whereas denitrifier-gene abundance correlated to organic matter content of the sediment, but not to nitrate concentrations. Our results show a mismatch in denitrification regulators at its different organizational scales. Denitrifier abundance is mostly regulated at within-ditch scales, whereas N-loads, regulated by landscape factors, are most important determinants of instantaneous denitrification rates.
机译:排水沟是农业景观的无处不在的尚未被忽视的特征。氮污染破坏了排水沟生态系统的营养平衡,以及它们排出的水上含水剂。反硝化可以通过将反应性氮转化为二氮气来改善抗施氮的影响。然而,影响排水沟中脱氮的因素仍然很差。在这项研究中,我们测试了沟渠内和区域环境条件如何影响反硝化偶联活动,丰度和社区结构,以了解多种尺度反硝化的控制。为此,我们在13个排水沟中以不同类型的沉积物,植被和土地利用为特征的13个引流沟渠量化。我们确定了利用NIR,NIRK和NOSZ基因作为代理的存在的反硝化率如何涉及反硝基丰度和社区结构。剥离率在沟渠之间广泛变化,范围为0.006至24mmol n m(-2)h(-1)。浮萍覆盖的沟渠,它包含高硝酸盐浓度并具有精细的含沙沉积物,是反硝化热点。我们在耕地旁边的沟渠中找到了最高的速度,然后是草原的沟渠;在泥炭地和自然保护区中观察到最低利率。反硝化与硝酸盐浓度相关,但不是Nirk,Nirs和NoSz丰度,而非硝基 - 基因丰富与沉积物的有机物质含量相关,但不是硝酸盐浓度。我们的结果在其不同的组织尺度上显示了脱氮调节器中的不匹配。退役大量大多数在沟渠内部受到调节,而通过景观因素调节的N负载是最重要的反硝化率的最重要决定因素。

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