Polyols and glucose particulate species as tracers of primary biogenic organic aerosols at 28 French sites
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Published:2019-03-15
Issue:5
Volume:19
Page:3357-3374
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Samaké Abdoulaye, Jaffrezo Jean-Luc, Favez Olivier, Weber SamuëlORCID, Jacob Véronique, Albinet AlexandreORCID, Riffault VéroniqueORCID, Perdrix Esperanza, Waked Antoine, Golly Benjamin, Salameh Dalia, Chevrier Florie, Oliveira Diogo Miguel, Bonnaire Nicolas, Besombes Jean-Luc, Martins Jean M. F., Conil Sébastien, Guillaud Géraldine, Mesbah Boualem, Rocq Benoit, Robic Pierre-Yves, Hulin Agnès, Le Meur Sébastien, Descheemaecker Maxence, Chretien Eve, Marchand NicolasORCID, Uzu GaëlleORCID
Abstract
Abstract. A growing number of studies
are using specific primary sugar species, such as sugar alcohols or primary saccharides,
as marker compounds to characterize and apportion primary biogenic organic aerosols
(PBOAs) in the atmosphere. To better understand their annual cycles, as well as their
spatiotemporal abundance in terms of concentrations and sources, we conducted a large
study focusing on three major atmospheric primary sugar compounds (i.e., arabitol,
mannitol, and glucose) measured in various environmental conditions for about 5300 filter
samples collected at 28 sites in France. Our results show significant atmospheric
concentrations of polyols (defined here as the sum of arabitol and mannitol) and glucose
at each sampling location, highlighting their ubiquity. Results also confirm that polyols
and glucose are mainly associated with the coarse rather than the fine aerosol mode. At
nearly all sites, atmospheric concentrations of polyols and glucose display a well-marked
seasonal pattern, with maximum concentrations from late spring to early autumn, followed
by an abrupt decrease in late autumn, and a minimum concentration during wintertime. Such
seasonal patterns support biogenic emissions associated with higher biological metabolic
activities (sporulation, growth, etc.) during warmer periods. Results from a previous
comprehensive study using positive matrix factorization (PMF) based on an extended
aerosol chemical composition dataset of up to 130 species for 16 of the same sample
series have also been used in the present work. The polyols-to-PMPBOA ratio
is 0.024±0.010 on average for all sites, with no clear distinction between traffic,
urban, or rural typology. Overall, even if the exact origin of the PBOA source is still
under investigation, it appears to be an important source of particulate matter (PM),
especially during summertime. Results also show that PBOAs are significant sources of
total organic matter (OM) in PM10 (13±4 % on a yearly average, and up to
40 % in some environments in summer) at most of the investigated sites. The mean PBOA
chemical profile is clearly dominated by contribution from OM (78±9 % of the mass
of the PBOA PMF on average), and only a minor contribution from the dust class
(3±4 %), suggesting that ambient polyols are most likely associated with
biological particle emissions (e.g., active spore discharge) rather than soil dust
resuspension.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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