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Dry and Wet Deposition of Nitrogen Emitted in Buenos Aires City to Waters of de la Plata River

机译:布宜诺斯艾利斯市排放到德拉普拉塔河水域的氮的干湿沉降

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摘要

Dry and wet deposition of atmospheric nitrogen species (NO_2 and HNO_3) coming from nitrogen oxides emissions in Buenos Aires city to surface waters of de la Plata River were estimated. Atmospheric dispersion models DAUMOD-RD (v.2) and CALPUFF were applied to area and point sources, respectively. These models were run considering 1 year of hourly meteorological data. Emission information included a typical diurnal variation of area source emissions. Annual atmospheric nitrogen (N-NO_2+N-HNO_3) deposition to 1,763 km_2 of the river was 35,600 kg-N year~(-1). Dry deposition processes accounted for 89% of this value. The small contribution of wet deposition was a consequence of the very few cases (5%) of rain events during offshore wind conditions. Monthly dry deposition to 1,763 km of the river varied from 1,628 kg-N month ' in February to 3,799 kg-N month ' in December, following the monthly occurrence of offshore winds. Monthly wet deposition varied from 1 kg-N month~(-1) in June to 1,162 kg-N month~(-1) in February. These results came from the combination of favorable conditions for formation of HNO3 and the occurrence of precipitation during offshore wind situations. Spatial distribution of annual atmospheric N deposition showed a strong coastal gradient. Deposition values reached a maximum of 137.1 kg-N km~(-2) year~(-1) near the shoreline, which was reduced to the half at 4 km from the coast.
机译:估算了来自布宜诺斯艾利斯市的氮氧化物排放到德拉普拉塔河地表水的大气氮素(NO_2和HNO_3)的干湿沉降。大气色散模型DAUMOD-RD(v.2)和CALPUFF分别应用于面源和点源。运行这些模型时考虑了一年的每小时气象数据。排放信息包括面源排放的典型日变化。河流年平均氮(N-NO_2 + N-HNO_3)沉积到河流的1,763 km_2为(35,600 kg-N)年(-1)。干沉积工艺占该值的89%。湿沉降的贡献很小,这是由于近海风条件下极少发生降雨事件(5%)的结果。在每月出现海上风之后,每月的干沉降量从2月份的1,628 kg-N月,到12月的3,799 kg-N月,变化至河流的1,763 km。每月的湿沉降从6月的1 kg-N月〜(-1)到2月的1162 kg-N月〜(-1)不等。这些结果来自于形成HNO3的有利条件和海上风电条件下出现降水的结合。年度大气氮沉降的空间分布表现出强烈的沿海梯度。沉积值在海岸线附近最高达到137.1 kg-N km〜(-2)年〜(-1),在距海岸4 km处降至一半。

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