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Effects of lakes and reservoirs on annual river nitrogen, phosphorus, and sediment export in agricultural and forested landscapes

机译:湖泊和水库对农业和森林景观中河流氮,磷和泥沙输出的影响

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Recently, effects of lakes and reservoirs on river nutrient export have been incorporated into landscape biogeochemical models. Because annual export varies with precipitation, there is a need to examine the biogeochemical role of lakes and reservoirs over time frames that incorporate interannual variability in precipitation. We examined long-term (similar to 20years) time series of river export (annual mass yield, Y, and flow-weighted mean annual concentration, C) for total nitrogen (TN), total phosphorus (TP), and total suspended sediment (TSS) from 54 catchments in Wisconsin, USA. Catchments were classified as small agricultural, large agricultural, and forested by use of a cluster analysis, and these varied in lentic coverage (percentage of catchment lake or reservoir water that was connected to river network). Mean annual export and interannual variability (CV) of export (for both Y and C) were higher in agricultural catchments relative to forested catchments for TP, TN, and TSS. In both agricultural and forested settings, mean and maximum annual TN yields were lower in the presence of lakes and reservoirs, suggesting lentic denitrification or N burial. There was also evidence of long-term lentic TP and TSS retention, especially when viewed in terms of maximum annual yield, suggesting sedimentation during high loading years. Lentic catchments had lower interannual variability in export. For TP and TSS, interannual variability in mass yield was often 50% higher than interannual variability in water yield, whereas TN variability more closely followed water (discharge) variability. Our results indicate that long-term mass export through rivers depends on interacting terrestrial, aquatic, and meteorological factors in which the presence of lakes and reservoirs can reduce the magnitude of export, stabilize interannual variability in export, as well as introduce export time lags. Copyright (c) 2013 John Wiley & Sons, Ltd.
机译:最近,湖泊和水库对河流养分出口的影响已被纳入景观生物地球化学模型。由于年出口随着降水而变化,因此需要检查湖泊和水库的生物地球化学作用,随着时间的推移,占地面积纳入沉淀的际变量。我们审查了总氮(TN),总磷(TP)和全悬浮沉积物的长期(年批量产量,y和流量为年度浓度C)的长期(类似的20年)时间序列来自美国威斯康辛的54个集水区。流域被归类为小型农业,大型农业,并通过使用聚类分析,这些集群分析,这些覆盖范围各种各样多(包括河网的集水湖或水库水的百分比)。由于TP,TN和TSS的森林流域,出口的平均年出口和平均变异性(y和c)的出口(y和c)较高。在农业和森林环境中,在湖泊和储层的存在下,均值和最大年度TN产量较低,表明仍然是脱硝或埋葬。还有许可证的TP和TSS保留的证据,特别是当在最大年产量方面观察时,暗示高负荷年度沉淀。犹氏集水集团的出口际变量较低。对于TP和TSS,质量产量的续变性通常高于水收率的依赖性变异性,而TN变异性更接近水(放电)可变性。我们的研究结果表明,长期大规模通过河流依赖于互动的陆地,水生和气象因素,其中湖泊和水库的存在可以降低出口幅度,稳定出口际变量,以及引入出口时间滞后。版权所有(c)2013 John Wiley&Sons,Ltd。

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