4.7 Article

Annual cycle of hygroscopic properties and mixing state of the suburbanaerosol in Athens, Greece

Journal

ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 23, Issue 1, Pages 235-249

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-23-235-2023

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The hygroscopic properties of atmospheric aerosol in a suburban environment in Athens, Greece, were studied. The growth factor distribution probability density function (GF-PDF) and mixing state were determined using a hygroscopicity tandem differential mobility analyzer (HTDMA). The results showed distinct hygroscopic ranges, with a non- and/or slightly hygroscopic mode (GF < 1.12) and a moderately hygroscopic mode (GF > 1.12), indicative of local/urban emissions and background aerosol influences. Cluster analysis revealed the link between aerosol hygroscopicity and emission sources and formation processes. The findings suggest that particles of similar nature and origin were present across the 50 nm and 80 nm sizes.
The hygroscopic properties of atmospheric aerosol were investigated at a suburban environment in Athens, Greece, from August 2016 to July 2017. The growth factor distribution probability density function (GF-PDF) and mixing state were determined with a hygroscopicity tandem differential mobility analyser (HTDMA). Four dry particle sizes (D-0) were selected to be analysed in terms of their hygroscopic properties at 90 % relative humidity. The annual mean GFs for D-0 = 30, 50, 80 and 250 nm were found to be equal to 1.28, 1.11, 1.13 and 1.22, respectively. The hygroscopic growth spectra were divided into two distinct hygroscopic ranges: a non- and/or slightly hygroscopic mode (GF < 1.12) and a moderately hygroscopic mode (GF > 1.12), which are representative of a suburban environment influenced by local/urban emissions and background aerosol. The standard deviation sigma of the GF-PDF was employed as a measure of the mixing state of ambient aerosol. The 30 nm particles were mostly internally mixed, whereas larger particles were found to be externally mixed, either with a distinct bimodal structure or with partly overlapping modes. Cluster analysis on the hourly dry number size distributions was performed to identify the link between aerosol hygroscopicity and aerosol emission sources and formation processes. The size distributions were classified into five groups, with the mixed urban and regional background aerosol (67 %) and the fresh traffic-related particles from the neighbourhood urban area (15 %) accounting for more than 80 % of the results. The hygroscopic properties for 50 and 80 nm were found to be similar in all cases, indicating particles of similar nature and origin across these sizes. This was also confirmed through the modal analysis of the average number size distributions for each cluster; the 50 and 80 nm particles were found to belong to the same Aitken mode in most cases. The 250 nm particles (i.e. accumulation mode) were generally more hygroscopic than Aitken particles but less hygroscopic than the 30 nm particles (nuclei mode).

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