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Wet deposition and scavenging ratio of air pollutants during an extreme rainstorm in the North China Plain

机译:华北平原特大暴雨过程中空气污染物的湿沉降与清除率

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Atmospheric wet deposition plays an important role in the supply of nutrients and toxic substances to terrestrial and aquatic environments.Although long-term (e.g.annual,multi-year) wet deposition is recorded well,pronounced and short-term changes in precipitation chemistry are less well investigated.In the present study,the precipitation chemistry and scavenging ratio of air pollutants were observed during an extreme torrential rain event (325.6 mm at the observation site) that occurred over 19-21 July 2016 in the North China Plain (NCP).The scavenging ratio of particles showed a similar spatial distribution to that of the precipitation amount in the NCP,indicating the efficient removal of particulate matter due to the large amount and precipitation intensity of the storm.In addition,the scavenging ratio of water soluble ions was larger than that of organics and gaseous pollutants such as SO2 and NO2,likely due to their differences in water solubility.Consequently,raindrops incorporated more aerosol sulfate than gaseous compounds.Due to the heavy precipitation amount,almost all species in rainwater during this storm showed their lowest concentration but the highest flux compared with other rain events,indicating an important role played by this storm in terms of the substances received by the terrestrial and marine ecosystems of the region.However,the contribution of this storm to the annual chemical flux was lower than that of precipitation amount,indicating that the atmospheric compounds were scavenged below-cloud first and were then diluted by the cloud/rainwater.Future studies are needed in the context of the occurrence of extreme rainfall events in the NCP from the perspective of climate variability.%大气湿沉降是陆地和水体环境中营养成分和有毒物质的重要来源.以往湿沉降研究较多关注年尺度或年际变化,极端降水事件鲜见报道.通过实验观测,发现201 6年7月19-21日华北极端暴雨(北京观测站325.6 mm)有效清除了区域大气颗粒物,但不同化学成分被湿清除的效率存在差异(无机离子比有机物和气态污染物更容易被湿清除).此次极端降水铵盐和硝酸盐的湿沉降通量占北京全年的22%和4%,相当于青藏高原一年的氮沉降.考虑到气候背景下极端暴雨出现的频次,极端降水的生态环境影响需要更精细化的评估.
机译:大气湿沉降在向陆生和水生环境供应养分和有毒物质方面起着重要作用。尽管长期(例如,一年,多年)湿沉降记录良好,但降水化学的短期变化较少在本研究中,我们观察了2016年7月19日至21日在华北平原(NCP)发生的一次极端暴雨事件(观测地点为325.6毫米)期间的大气污染物的沉淀化学和清除率。颗粒物的清除率与NCP中的降水量呈相似的空间分布,这表明由于暴风雨的数量和降水强度大,有效清除了颗粒物。此外,水溶性离子的清除率是比有机物和气态污染物(例如SO2和NO2)更大,这可能是由于它们的水溶性不同。由于降水量大,与其他降雨事件相比,这场暴风雨期间雨水中几乎所有物种都表现出最低的浓度,但通量却最高,这表明暴风雨在物质上具有重要作用然而,这场风暴对年化学通量的贡献低于降水量,表明大气化合物首先被清除在云层以下,然后被云层稀释/从气候变化的角度来看,在NCP发生极端降雨事件的背景下,需要进行未来的研究。%大气湿空气是陆地和水体环境中营养和有毒物质的重要来源。通过实验观察,发现201 6年7月19-21日华北极端暴雨(北京观测站325.6 mm)有效清除了区域大气颗粒物,但不同化学极端极端铵盐和硝酸盐的湿气通量占北京大部分的22%和4%,相当于青藏高原一年的氮肥。考虑到气候背景下极端暴雨出现的频次,极端退化的生态环境影响需要更精细化的评估。

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