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Chemical Characterization of PM_(1-2.5) and its Associations with PM_1, PM_(2.5-10) and Meteorology in Urban and Suburban Environments

摘要


This study investigated the PM_(1-2.5) (the intermodal fraction of particulate matter) representing the transition area between the fine and coarse size ranges. Due to this characteristic, PM_(1-2.5) may contain particles from both modes. The aim of this work was to examine the associations between PM_(1-2.5) and the coarse (PM_(2.5-10))/fine (PM_1) fraction under different meteorological conditions at various sites in the Czech Republic during winter and summer. Size-resolved PM mass concentrations were determined and meteorological parameters recorded at an urban industrial and a suburban site in Ostrava during winter 2014 and at an urban traffic site and a suburban site in Prague during summer 2014 and winter 2015. The influence of sources producing the coarse/fine fraction on PM_(1-2.5) was investigated with an elemental composition analysis and an ion analysis (Ca^(2+)-representing PM_(2.5-10) and SO_4^(2-)-representing PM_1). During all campaigns, PM_(1-2.5) accounted for 1-26% of PM_(10). In winter, crustal elements (Si, Fe, and Ca) significantly influenced the coarse fraction and even PM_(1-2.5) at all sites, while sulfur was significant in PM_(1-2.5) and the fine fraction at suburban sites. The median SO_4^(2-) concentration was higher than the Ca^(2+) concentration in PM_(1-2.5) at all sites, except the industrial site, due to a specific source. The increased SO_4^(2-) amount in PM_(1-2.5) was also observed in summer during rainy days (Prague urban site). In summer, crustal elements were important in both PM_(1-2.5) and the coarse fraction, while S still dominated in PM_1. Median SO_4^(2-) concentrations in PM_(1-2.5) and the coarse fraction were significantly lower than in winter. The enrichment factors and wind speed-direction analysis helped to reveal potential air pollution sources. To conclude, according to the performed analyses, PM_(1-2.5) was influenced by the sources of the coarse fraction during all campaigns. The additional significant influence of sources producing the fine fraction was evident under increased relative humidity conditions.

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