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Global Pollution of Surface Waters from Point and Nonpoint Sources of Nitrogen

机译:点状和非点状氮源对地表水的全球污染

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摘要

Global 0.5- by 0.5-degree resolution estimates are presented on the fate of nitrogen (N) stemming from point and nonpoint sources, including plant uptake, denitrification, leaching from the rooting zone, rapid flow through shallow groundwater, and slow flow through deep groundwater to riverine systems. Historical N inputs are used to describe the N flows in groundwater. For nonpoint N sources (agricultural and natural ecosystems), calculations are based on local hydrology, climate, geology, soils, climate and land use combined with data for 1995 on crop production, N inputs from N fertilizers and animal manure, and estimates for ammonia emissions, biological N fixation, and N deposition. For point sources, our estimates are based on population densities and human N emissions, sanitation, and treatment. The results provide a first insight into the magnitude of the N losses from soil-plant systems and point sources in various parts of the world, and the fate of N during transport in atmosphere, groundwater, and surface water. The contribution to the river N load by anthropogenic N pollution is dominant in many river basins in Europe, Asia, and North Africa. Our model results explain much of the variation in measured N export from different world river basins.
机译:对源自点和非点源的氮(N)命运(包括植物吸收,反硝化,从生根区浸出,快速流过浅层地下水和缓慢流过深层地下水)的命运提出了全球0.5至0.5度的分辨率估算值到河流系统。历史N输入用于描述地下水中N的流量。对于非点源氮(农业和自然生态系统),计算是基于当地水文学,气候,地质,土壤,气候和土地利用,结合1995年作物产量,氮肥和动物粪便的氮投入以及氨的估算数据排放,生物固氮和氮沉积。对于点源,我们的估计是基于人口密度和人类氮排放,卫生设施和治疗的。这些结果提供了对世界各地土壤-植物系统和点源氮损失量的初步了解,以及在大气,地下水和地表水运输过程中氮的命运。在欧洲,亚洲和北非的许多流域中,人为氮污染对河流氮负荷的贡献占主导地位。我们的模型结果解释了来自世界不同流域的测得氮出口量的大部分变化。

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