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Global modeling of the fate of nitrogen from point and nonpoint sources in soils, groundwater, and surface water

机译:土壤,地下水和地表水中点源和非点源氮的命运的全局模型

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摘要

[1] We present a global model that describes the fate of nitrogen (N) from point and nonpoint sources in the hydrological system up to the river mouths at the 0.5° by 0.5° spatial and annual temporal resolution. Estimates for point sources are based on population densities, per capita human N emissions, and data on sanitation coverage and wastewater treatment. For nonpoint sources, we use spatial information on land use, climate, hydrology, geology, and soils, combined with data on N inputs (fertilizers and animal manure, biological N fixation, and atmospheric deposition), and outputs (N removal in harvested agricultural products, ammonia emissions). Denitrification in the root zone and nitrate leaching to groundwater are calculated with a model that combines the effect of temperature, crop type, soil properties, and hydrological conditions. The nitrate concentration of the outflow for shallow and deep groundwater layers is based on historical inputs of fertilizer N and the effects of residence time and denitrification. In-stream N retention is based on a global estimate of 30% of the N discharged to surface water. Calculated and reported total N concentrations of discharge near the river outlet agree fairly well. However, our model systematically overestimates total N concentrations for river basins with mean annual temperature > 0℃.
机译:[1]我们提出了一个全球模型,该模型描述了水文系统中点源和非点源的氮(N)的命运,时空分辨率和年际分辨率分别为0.5°x 0.5°。点源的估算是基于人口密度,人均人均氮排放量以及有关卫生覆盖率和废水处理的数据。对于非点源,我们使用有关土地利用,气候,水文,地质和土壤的空间信息,并结合氮输入(肥料和动物粪便,生物固氮和大气沉降)和输出(收获的农业作物中的氮去除)的数据产品,氨气排放)。通过结合温度,作物类型,土壤特性和水文条件影响的模型来计算根区的反硝化和硝酸盐向地下水的淋溶。浅层和深层地下水流出物中的硝酸盐浓度基于肥料N的历史输入以及停留时间和反硝化作用的影响。流中氮的保留量是基于对排放到地表水中的氮总量的30%的总体估算得出的。计算和报告的河口附近总氮排放浓度相当吻合。但是,我们的模型系统地高估了年平均温度> 0℃的流域的总氮浓度。

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