{"title":"Atmospheric Organic Aerosol Age Distribution over Europe during a Period with Intense Wildfires","authors":"Ksakousti Skyllakou, Petro Uruci, Spyros Pandis","doi":"10.1021/acsestair.6c00040","DOIUrl":null,"url":null,"abstract":"<p>The age of particulate matter (PM), focusing on organic\r\naerosols,\r\nwas estimated during a summer period with severe wildfires in Europe,\r\ncombining a chemical transport model (CTM) with a computationally\r\nefficient source apportionment algorithm. The organic components of\r\nPM were highly aged, especially when they originated from wildfires.\r\nThe average age of organic aerosol (OA) at the ground level above\r\nEurope was 58 h, while the average age of biomass burning organic\r\naerosol (bbOA) was 86 h, and that of non-bbOA was 49 h. The average\r\nage of OA was different for OA species with different volatilities.\r\nAs the volatility of the OA components decreased, their average age\r\nincreased. The average age of the semivolatile biomass burning secondary\r\nOA was 66 h, while that of low volatility biomass burning secondary\r\nOA was 95 h. These results suggest that the OA to which the population\r\nof Europe is exposed is quite different due to aging physical and\r\nchemical processes from the particles emitted by its various sources.\r\nThe average age of OA was found to decrease when the OH levels increased\r\nand vice versa. A reduction of the aging rate by an order of magnitude\r\nresulted in a 45% increase in the average age of anthropogenic secondary\r\nOA. On the other hand, 10 times faster aging reactions resulted in\r\na 20% decrease in the average age of anthropogenic secondary organic\r\naerosol. These changes resulted in minor changes in the average age\r\nof the primary organic aerosol.</p>","PeriodicalId":100014,"journal":{"name":"ACS ES&T Air","volume":"3 9","pages":"2225–2235"},"PeriodicalIF":0.0000,"publicationDate":"2026-09-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"ACS ES&T Air","FirstCategoryId":"1085","ListUrlMain":"https://pubs.acs.org/doi/10.1021/acsestair.6c00040","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2026/8/10 0:00:00","PubModel":"Epub","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The age of particulate matter (PM), focusing on organic
aerosols,
was estimated during a summer period with severe wildfires in Europe,
combining a chemical transport model (CTM) with a computationally
efficient source apportionment algorithm. The organic components of
PM were highly aged, especially when they originated from wildfires.
The average age of organic aerosol (OA) at the ground level above
Europe was 58 h, while the average age of biomass burning organic
aerosol (bbOA) was 86 h, and that of non-bbOA was 49 h. The average
age of OA was different for OA species with different volatilities.
As the volatility of the OA components decreased, their average age
increased. The average age of the semivolatile biomass burning secondary
OA was 66 h, while that of low volatility biomass burning secondary
OA was 95 h. These results suggest that the OA to which the population
of Europe is exposed is quite different due to aging physical and
chemical processes from the particles emitted by its various sources.
The average age of OA was found to decrease when the OH levels increased
and vice versa. A reduction of the aging rate by an order of magnitude
resulted in a 45% increase in the average age of anthropogenic secondary
OA. On the other hand, 10 times faster aging reactions resulted in
a 20% decrease in the average age of anthropogenic secondary organic
aerosol. These changes resulted in minor changes in the average age
of the primary organic aerosol.