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The concentration, source and deposition flux of ammonium and nitrate in atmospheric particles during dust events at a coastal site in northern China

机译:中国北方沿海地区扬尘事件中大气颗粒物中铵和硝酸盐的浓度,来源和沉积通量

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摘要

Asian dust has been reported to carry anthropogenic reactivenitrogen during transport from source areas to the oceans. In this study, weattempted to characterize NH and NO in atmosphericparticles collected at a coastal site in northern China during spring dustevents from 2008 to 2011. Based on the mass concentrations of NHand NO in each total suspended particle (TSP) sample, the samplescan be classified into increasing or decreasing types. In Category 1, theconcentrations of NH and NO were 20–440 % higherin dust day samples relative to samples collected immediately before or aftera dust event. These concentrations decreased by 10–75 % in the dust daysamples in Categories 2 and 3. Back trajectory analysis suggested thatmultiple factors, such as the transport distance prior to the reception site,the mixing layer depth on the transport route and the residence time acrosshighly polluted regions, might affect the concentrations of NH andNO. NH in the dust day samples was likely either in theform of ammonium salts existing separately to dust aerosols or as theresidual of incomplete reactions between ammonium salts and carbonate salts.NO in the dust day samples was attributed to various formationprocesses during the long-range transport. The positive matrix factorization(PMF) receptor model results showed that the contribution of soil dustincreased from 23 to 36 % on dust days, with decreasing contributionsfrom local anthropogenic inputs and associated secondary aerosols. Theestimated deposition flux of N varied greatly from event toevent; e.g., the dry deposition flux of N increased by9–285 % in Category 1 but decreased by 46–73 % in Category 2. InCategory 3, the average dry deposition fluxes of particulate nitrate andammonium decreased by 46 % and increased by 10 %, respectively, leadingto 11–48 % decrease in the fluxes of N.
机译:据报道,亚洲尘埃在从源区到海洋的运输过程中会携带人为的活性氮。在这项研究中,我们试图表征2008年至2011年春季沙尘暴事件期间在中国北方沿海站点收集的大气颗粒中的NH和NO。基于每个总悬浮颗粒(TSP)样品中NHand NO的质量浓度,可以对样品进行分类分为增加或减少类型。在类别1中,沙尘日样品中的NH和NO浓度比粉尘事件发生之前或之后立即采集的样品高20-440%。在类别2和类别3的尘埃日样本中,这些浓度降低了10–75%。反向轨迹分析表明,多个因素,例如接收点之前的运输距离,运输路线上的混合层深度以及在高污染区域的停留时间可能会影响NH和NO的浓度。尘埃日样品中的NH可能是铵盐形式存在于粉尘气溶胶中,也可能是铵盐与碳酸盐之间不完全反应的残留物。尘埃日样品中的NO归因于远距离运输过程中的各种形成过程。正矩阵分解(PMF)受体模型的结果表明,在沙尘天,土壤尘埃的贡献从23%增加到36%,而本地人为输入和相关的次级气溶胶的贡献则减少。估计的N沉积通量因事件而异。例如,第1类中N的干沉降通量增加了9–285%,而第2类中的干沉降通量减少了46–73%。在类别3中,硝酸盐和铵颗粒的平均干沉降通量分别减少了46%和增加了10%。 ,导致氮通量下降11–48%。

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