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Sub-micron atmospheric aerosols in the surroundings of Marseille and Athens: physical characterization and new particle formation

机译:马赛和雅典环境中的亚微米大气气溶胶:物理特征和新颗粒形成

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The properties of atmospheric aerosol particles in Marseille and Athenswere investigated. The studies were performed in Marseille, France,during July 2002 and in Athens, Greece, during June 2003. The aerosolsize distribution and the formation and growth rates of newly formedparticles were characterized using Differential Mobility ParticleSizers. Hygroscopic properties were observed using a Hygroscopic TandemDifferential Mobility Analyzer setup. During both campaigns, theobservations were performed at suburban, almost rural sites, and thesites can be considered to show general regional background behaviordepending on the wind direction. At both sites there were clear patternfor both aerosol number concentration and hygroscopic properties.Nucleation mode number concentration increased during the morning hoursindicating new particle formation, which was observed during more than30% of the days. The observed formation rate was typically more than1 cm−3 s−1, and the growth rate was between1.2–9.9 nm h−1. Based on hygroscopicity measurements in Athens,the nucleation mode size increase was due to condensation of both waterinsoluble and water soluble material. However, during a period of lessanthropogenic influence, the growth was to a larger extent due to waterinsoluble components. When urban pollution was more pronounced, growthdue to condensation of water soluble material dominated.
机译:研究了马赛和雅典的大气气溶胶颗粒的特性。该研究于2002年7月在法国马赛和2003年6月在希腊雅典进行。使用差动迁移粒度仪对气溶胶的分布以及新形成的颗粒的形成和生长速率进行了表征。使用吸湿串联差动分析仪设置观察吸湿性能。在这两次运动期间,观测都是在郊区,几乎是农村的地点进行的,这些地点可以视为根据风向显示一般的区域背景行为。在两个站点上,气溶胶数浓度和吸湿性都有清晰的模式。早上数小时内成核模式数浓度增加,表明有新的颗粒形成,在30%的时间内观察到。观察到的形成速率通常大于1 cm -3 s -1 ,生长速率在1.2–9.9 nm h -1 之间。根据雅典的吸湿性测量,成核模式尺寸的增加是由于水不溶性物质和水溶性物质的凝结所致。然而,在较少的人为影响期间,由于水不溶性成分,其生长在较大程度上。当城市污染更加明显时,由于水溶性物质的凝结而增长。

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