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Nitrogen retention in wetlands, lakes and rivers

机译:湿地,湖泊和河流中的氮保留

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As human activities continue to alter the global nitrogen cycle, the ability to predict the impact of increased nitrogen loading to freshwater systems is becoming more and more important. Nitrogen retention is of particular interest because it is through its combined processes (denitrification, nitrogen sedimentation and uptake by aquatic plants) that local and downstream nitrogen concentrations are reduced. Here, we compare the magnitude of nitrogen retention and its components in wetlands, lakes and rivers. We show that wetlands retain the highest proportion of total nitrogen loading, followed by lakes and then rivers. The differences in the proportion of N retained among systems is explained almost entirely by differences in water discharge. Denitrification is the primary mechanism of nitrogen retention, followed by nitrogen sedimentation and uptake by aquatic plants.
机译:随着人类活动继续改变全球氮循环,预测增加氮负荷对淡水系统的影响的能力变得越来越重要。氮保留特别受关注,因为它是通过其结合的过程(脱氮,氮沉降和水生植物吸收)而降低了局部和下游氮的浓度。在这里,我们比较了湿地,湖泊和河流中氮的保留量及其组成。我们表明,湿地在总氮负荷中所占比例最高,其次是湖泊,然后是河流。系统之间保留的氮比例的差异几乎完全由排水量的差异来解释。反硝化作用是氮保留的主要机理,其次是氮沉降和水生植物吸收氮。

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