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Nitrogen retention in a river system and the effects of river morphology and lakes

机译:氮在河流系统中的保留以及河流形态和湖泊的影响

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The mean annual transfer (loss and retention) of nitrogen in a river system was estimated using a conceptual approach based on water surface area and runoff. Two different approaches for the calculation of water surface area were applied to determine riverine nitrogen retention in four European catchments, ranging between 860-14,000 km(2) in area, and differing considerably in the proportion and distribution of surface waters, specific runoff and specific nutrient emissions. The transfer rate was estimated sequentially as either the mean value for the total catchment, on a sub-catchment scale, or considering the distribution of water surface area within a sub-catchment. For the latter measure, nitrogen retention in larger lakes was calculated separately. Nitrogen emissions modelled with MONERIS and HBV-N were used to calculate nitrogen river loads and compare those with observed loads. Inclusion of the proportion of water area within a sub-catchment improved modelled results in catchment with large lakes in sub-catchments, but not where there was a homogenous distribution of surface waters among sub-catchments.
机译:使用基于水表面积和径流量的概念性方法估算了河流系统中氮的年均转移量(损失和保留量)。应用了两种不同的计算水表面积的方法来确定四个欧洲集水区的河流氮保留量,范围在860-14,000 km(2)之间,并且在地表水的比例和分布,特定径流和特定比例方面存在很大差异。营养物排放。依次估算迁移率,将其作为子集水规模的总集水量的平均值,或者考虑子集水区内的水表面积分布。对于后一种措施,分别计算了较大湖泊中的氮保留量。用MONERIS和HBV-N建模的氮排放量用于计算氮河负荷并将其与观测负荷进行比较。将子集水区中的水面积比例包括在内,可以改善模拟结果,使子集水区中有大湖,但子集水区之间的地表水分布不均匀。

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