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Precipitation chemistry and atmospheric nitrogen deposition at a rural site in Beijing, China

机译:中国北京某乡村地区的降水化学和大气氮沉降

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Precipitation chemistry and atmospheric nitrogen (N) deposition are of great concern worldwide due to their close relationships with air quality and impacts on ecosystems. However, evaluation of the chemical composition of precipitation and N deposition flux in rural areas of Beijing has received little attention to date. This paper presents the chemical constituents, possible sources and wet deposition fluxes of water-soluble ions (NH4+, NO3- SO42-, Cl-, Na+, K+, Ca2+, Mg2+) in precipitation samples collected during 2017-2018 at a rural site located at northwest of Beijing city; meanwhile, dry deposition of reactive N species (gaseous ammonia, nitrogen dioxide, nitric acid, and particulate (p) NH4+ and NO3-) were also quantified. During this 2-year period, the volume-weighted mean (VWM) pH of precipitation was 6.73, and all samples had pH values above 6.0. The VWM electric conductivity of precipitation and the mean sum of all measured ions was 43.8 mu S cm(-1) and 591.9 mu eq L-1, respectively, indicating a significant impact of atmospheric pollution. Ca2+ and NH4+ were the dominant neutralizing species for precipitation acidity. Positive matrix factorization analysis further confirmed five sources for water-soluble ions, including sea salt aging, secondary formation, agriculture, crust, and biomass burning. The annual mean wet N deposition was 4.6, 3.4 and 8.0 kg N ha(-1) yr(-1) for NH4+, NO3- and total inorganic N, respectively. The total dry N deposition was dominated by gaseous ammonia (11.5 kg N ha(-1) yr(-1)). The total N deposition (wet plus dry) was 27.7 kg N ha(-1) yr(-1), where dry deposition contributed to 75% and wet deposition 25% of the total. The simulations from the GEOS-Chem model indicate that agricultural (fertilizer use and livestock) and nonagricultural sources (industry, power plant, and transportation) are both important contributors to total N deposition. These results could be useful in evaluating/developing emission control policies to protect the eco-environment in Beijing.
机译:由于降水化学和大气中的氮与空气质量密切相关,并且对生态系统造成影响,因此在全球范围内受到极大关注。然而,迄今为止,对北京农村地区降水的化学成分和氮沉降通量的评价一直很少受到关注。本文介绍了2017-2018年在一个农村地点收集的降水样品中水溶性离子(NH4 +,NO3-SO42-,Cl-,Na +,K +,Ca2 +,Mg2 +)的化学成分,可能的来源和湿沉降通量在北京市西北;同时,还量化了反应性N物质(气态氨,二氧化氮,硝酸和(p)NH4 +和NO3-颗粒)的干沉降。在这两年期间,降水的体积加权平均(VWM)pH为6.73,所有样品的pH值均超过6.0。降水的VWM电导率和所有测得离子的平均总和分别为43.8μS cm(-1)和591.9μeqeq L-1,表明对大气污染的影响很大。 Ca2 +和NH4 +是沉淀酸度的主要中和物质。积极的矩阵分解分析进一步确认了水溶性离子的五个来源,包括海盐老化,二次形成,农业,地壳和生物质燃烧。对于NH4 +,NO3-和总无机N,年平均湿N沉积量分别为4.6、3.4和8.0 kg N ha(-1)yr(-1)。总的干氮沉积以气态氨(11.5 kg N ha(-1)yr(-1))为主。 N沉积总量(湿加干)为27.7 kg N ha(-1)yr(-1),其中干沉积占总量的75%,湿沉积占总量的25%。 GEOS-Chem模型的模拟表明,农业(肥料使用和畜牧业)和非农业来源(工业,发电厂和运输业)都是总氮沉积的重要因素。这些结果可能有助于评估/制定保护北京生态环境的排放控制政策。

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