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Influences of the 2010 Eyjafjallaj?kull volcanic plume on air quality in the northern Alpine region

机译:2010年Eyjafjallaj的影响?KULL VOLCANIC PLUME在北高山地区空气质量

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A series of major eruptions of the Eyjafjallaj?kull volcano in Iceland started on 14 April 2010 and continued until the end of May 2010. The volcanic emissions moved over nearly the whole of Europe and were observed first on 16 April 2010 in Southern Germany with different remote sensing systems from the ground and space. Enhanced PM10 and SO2 concentrations were detected on 17 April at mountain stations (Zugspitze/Schneefernerhaus and Schauinsland) as well as in Innsbruck by in situ measurement devices. On 19 April intensive vertical mixing and advection along with clear-sky conditions facilitated the entrainment of volcanic material down to the ground. The subsequent formation of a stably stratified lower atmosphere with limited mixing near the ground during the evening of 19 April led to an additional enhancement of near-surface particle concentrations. Consequently, on 19 April and 20 April exceedances of the daily threshold value for particulate matter (PM10) were reported at nearly all monitoring stations of the North Alpine foothills as well as at mountain and valley stations in the northern Alps. The chemical analyses of ambient PM10 at monitoring stations of the North Alpine foothills yielded elevated Titanium concentrations on 19/20 April which prove the presence of volcanic plume material. Following this result the PM10 threshold exceedances are also associated with the volcanic plume. The entrainment of the volcanic plume material mainly affected the concentrations of coarse particles (1 μm) – interpreted as volcanic ash – and ultrafine particles (100 nm), while the concentrations of accumulation mode aerosol (0.1–1 μm) were not changed significantly. With regard to the occurrence of ultrafine particles, it is concluded that their formation was triggered by high sulphuric acid concentrations which are necessarily generated by the photochemical processes in a plume rich in sulphur dioxide under high solar irradiance. It became evident that during the course of several days, the Eyjafjallaj?kull volcanic emissions influenced the near-surface atmosphere and thus the ambient air quality. Although the volcanic plume contributed to the overall exposure of the population of the northern Alpine region on two days, only minor effects on the exacerbation of respiratory and cardiovascular symptoms can be expected.
机译:Eyjafjallaj的一系列主要爆发?冰岛的Kull火山于2010年4月14日开始,持续到2010年5月底。火山的排放迁移到近期欧洲,并于2010年4月16日在德国南部举办了不同从地面和空间遥感系统。在4月17日在山站(Zugspitze / Schneefernerhaus和Schauinsland)以及原位测量装置的Innsbruck中检测到增强的PM10和SO2浓度。 4月19日,强化垂直混合和平流以及明确的条件,便于将火山材料夹紧到地面。随后在4月19日晚上,在地面附近形成了稳定分层的较低气氛,导致了近表面颗粒浓度的额外增强。因此,4月19日和4月20日的颗粒物质(PM10)的每日阈值的超标于北高山山麓以及北阿尔卑斯北部的山地和山谷站。环境PM10在北高山山麓的监测站的化学分析产生了19/20 4月的钛浓度升高,证明了火山羽毛材料的存在。在此结果之后,PM10阈值的超标也与火山羽流相关。火山羽流料的夹带主要影响粗颗粒(>1μm)的浓度 - 解释为火山灰和超细颗粒(100nm),而积累模式气溶胶(0.1-1μm)的浓度不会显着变化。关于超细颗粒的发生,得出结论,它们的形成由高硫酸浓度引发,该高硫酸浓度是在高太阳辐照度下富含二氧化硫的光化学方法产生的。显而易见的是,在几天的过程中,Eyjafjallaj?kull火山排放影响了近表面气氛,从而影响了环境空气质量。虽然火山羽毛在两天内促成了北高山地区人口的总体暴露,但只能预期对呼吸系统和心血管症状的加剧的轻微影响。
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