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首页> 外文期刊>The Science of the Total Environment >Denitrification and benthic metabolism in lowland pit lakes: The role of trophic conditions
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Denitrification and benthic metabolism in lowland pit lakes: The role of trophic conditions

机译:低地坑湖中的反硝化和底栖代谢:营养局的作用

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Over recent decades, a great number of pit lakes have been formed, as a result of sand and gravel quarrying in river floodplains that are often also heavily exploited for agriculture. These lakes can act as nutrient filters and regulate the nitrogen pollution resulting from agricultural fertiliser use. In this paper we report the main outcomes of a study of the major nitrogen pathways in five pit lakes of differing trophic status, located along a lowland stretch of the Po river (Northern Italy). Benthic nitrogen fluxes and denitrification rates were determined in the hypolimnion and denitrification and reactive nitrogen assimilation by microphytobenthos in the littoral zone. We tested the hypothesis that lake depth and trophic status can impair denitrification and/or reactive nitrogen assimilation, compromising the function of the lakes as nutrient filters. In the studied lakes, denitrification and reactive nitrogen assimilation by primary producer communities accounted for substantial nitrogen removal rates, which were among the highest reported in the literature. Benthic nitrogen fluxes and denitrification varied between and within lakes, with depth. The littoral zone and surface waters also supported primary production, favouring nitrogen assimilation and temporal retention in the primary producer biomass. In all lakes, denitrification rates decreased from littoral to hypolimnetic sites. Denitrification rates and net nitrogen assimilation also diminished from oligotrophic to eutrophic conditions. To some extent, in eutrophic lakes there was a transfer of primary production from the benthos to the water column and the benthic system became heterotrophic, reducing the capacity for net nitrogen removal.
机译:近几十年来,由于河流泛滥平坦的沙子和砾石采石,往往也是大量剥削农业的河流和砾石采石。这些湖泊可作为营养过滤器并调节由农业肥料使用引起的氮污染。在本文中,我们报告了在沿着PO河(意大利北部)的低地延伸的不同营养状况的五个坑湖中的主要氮途径研究的主要结果。在沿着沿壁带中的微细胞脱硫和脱氮和反硝化和反应性氮气同化中测定了底栖氮气通量和脱氮率。我们测试了湖泊深度和营养状况可能会损害反硝化和/或反应性氮同化的假设,损害湖泊作为营养过滤器的功能。在研究的湖泊中,初级生产者社区的反硝化和反应性氮同化占氮气去除率的大量氮气去除率,这是文献中最高报道的。底栖氮气助熔剂和脱氮在湖泊之间,深度变化。沿波特区和地表水也支持初级生产,有利于初级生产者生物质中的氮同化和时间保留。在所有湖泊中,脱硝率从沿碱性到低血管位点下降。脱硝率和净氮同化也从抗营养术中减少到富营养化条件下。在某种程度上,在富营养的湖泊中,将初级生产转移到水柱上,底氏系统变得异养,降低了净氮去除的能力。

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