Chemical evolution of primary and secondary biomass burning aerosols during daytime and nighttime
<p>Primary emissions from wood and pellet stoves were aged in an atmospheric simulation chamber under daytime and nighttime conditions. The aerosol was analyzed with online aerosol mass spectrometry and offline Fourier transform infrared spectroscopy (FTIR). Measurements using the two techniqu...
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Copernicus Publications
2023-07-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | https://acp.copernicus.org/articles/23/7461/2023/acp-23-7461-2023.pdf |
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author | A. Yazdani S. Takahama J. K. Kodros M. Paglione M. Paglione M. Masiol S. Squizzato K. Florou C. Kaltsonoudis S. D. Jorga S. N. Pandis S. N. Pandis A. Nenes A. Nenes |
author_facet | A. Yazdani S. Takahama J. K. Kodros M. Paglione M. Paglione M. Masiol S. Squizzato K. Florou C. Kaltsonoudis S. D. Jorga S. N. Pandis S. N. Pandis A. Nenes A. Nenes |
author_sort | A. Yazdani |
collection | DOAJ |
description | <p>Primary emissions from wood and pellet stoves were aged in an atmospheric simulation chamber under daytime and nighttime conditions. The aerosol was analyzed with online aerosol mass spectrometry and offline Fourier transform infrared spectroscopy (FTIR). Measurements using the two techniques agreed reasonably well in terms of the organic aerosol (OA) mass concentration, <span class="inline-formula">OA:OC</span> trends, and concentrations of biomass burning markers – lignin-like compounds and anhydrosugars. Based on aerosol mass spectrometry, around 15 % of the primary organic aerosol (POA) mass underwent some form of transformation during daytime oxidation conditions after 6–10 h of atmospheric exposure. A lesser extent of transformation was observed during the nighttime oxidation. The decay of certain semi-volatile (e.g., levoglucosan) and less volatile (e.g., lignin-like) POA components was substantial during aging, highlighting the role of heterogeneous reactions and gas–particle partitioning. Lignin-like compounds were observed to degrade under both daytime and nighttime conditions, whereas anhydrosugars degraded only under daytime conditions. Among the marker mass fragments of primary biomass burning OA (bbPOA), heavy ones (higher <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>m</mi><mo>/</mo><mi>z</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="63c7f3946b001d4e8415de9c4a1834dd"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-7461-2023-ie00001.svg" width="23pt" height="14pt" src="acp-23-7461-2023-ie00001.png"/></svg:svg></span></span>) were relatively more stable during aging. The biomass burning secondary OA (bbSOA) became more oxidized with continued aging and resembled that of aged atmospheric organic aerosols. The bbSOA formed during daytime oxidation was dominated by acids. Organonitrates were an important product of nighttime reactions in both humid and dry conditions. Our results underline the importance of changes to both the primary and secondary biomass burning aerosols during their atmospheric aging. Heavier fragments from aerosol mass spectrometry seldom used in atmospheric chemistry can be used as more stable tracers of bbPOA and, in combination with the established levoglucosan marker, can provide an indication of the extent of bbPOA aging.</p> |
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language | English |
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spelling | doaj.art-b1a37e8873274fe39a78b92f5c295f1f2023-07-10T07:57:12ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242023-07-01237461747710.5194/acp-23-7461-2023Chemical evolution of primary and secondary biomass burning aerosols during daytime and nighttimeA. Yazdani0S. Takahama1J. K. Kodros2M. Paglione3M. Paglione4M. Masiol5S. Squizzato6K. Florou7C. Kaltsonoudis8S. D. Jorga9S. N. Pandis10S. N. Pandis11A. Nenes12A. Nenes13Laboratory of Atmospheric Processes and their Impacts (LAPI), ENAC/IIE, Ecole polytechnique fédérale de Lausanne (EPFL), Lausanne, SwitzerlandLaboratory of Atmospheric Processes and their Impacts (LAPI), ENAC/IIE, Ecole polytechnique fédérale de Lausanne (EPFL), Lausanne, SwitzerlandInstitute for Chemical Engineering Sciences, Foundation for Research and Technology Hellas (ICE-HT/FORTH), Patras, GreeceInstitute for Chemical Engineering Sciences, Foundation for Research and Technology Hellas (ICE-HT/FORTH), Patras, GreeceItalian National Research Council – Institute of Atmospheric Sciences and Climate (CNR-ISAC), Bologna, ItalyInstitute for Chemical Engineering Sciences, Foundation for Research and Technology Hellas (ICE-HT/FORTH), Patras, GreeceInstitute for Chemical Engineering Sciences, Foundation for Research and Technology Hellas (ICE-HT/FORTH), Patras, GreeceInstitute for Chemical Engineering Sciences, Foundation for Research and Technology Hellas (ICE-HT/FORTH), Patras, GreeceInstitute for Chemical Engineering Sciences, Foundation for Research and Technology Hellas (ICE-HT/FORTH), Patras, GreeceInstitute for Chemical Engineering Sciences, Foundation for Research and Technology Hellas (ICE-HT/FORTH), Patras, GreeceInstitute for Chemical Engineering Sciences, Foundation for Research and Technology Hellas (ICE-HT/FORTH), Patras, GreeceDepartment of Chemical Engineering, University of Patras, Patras, GreeceLaboratory of Atmospheric Processes and their Impacts (LAPI), ENAC/IIE, Ecole polytechnique fédérale de Lausanne (EPFL), Lausanne, SwitzerlandInstitute for Chemical Engineering Sciences, Foundation for Research and Technology Hellas (ICE-HT/FORTH), Patras, Greece<p>Primary emissions from wood and pellet stoves were aged in an atmospheric simulation chamber under daytime and nighttime conditions. The aerosol was analyzed with online aerosol mass spectrometry and offline Fourier transform infrared spectroscopy (FTIR). Measurements using the two techniques agreed reasonably well in terms of the organic aerosol (OA) mass concentration, <span class="inline-formula">OA:OC</span> trends, and concentrations of biomass burning markers – lignin-like compounds and anhydrosugars. Based on aerosol mass spectrometry, around 15 % of the primary organic aerosol (POA) mass underwent some form of transformation during daytime oxidation conditions after 6–10 h of atmospheric exposure. A lesser extent of transformation was observed during the nighttime oxidation. The decay of certain semi-volatile (e.g., levoglucosan) and less volatile (e.g., lignin-like) POA components was substantial during aging, highlighting the role of heterogeneous reactions and gas–particle partitioning. Lignin-like compounds were observed to degrade under both daytime and nighttime conditions, whereas anhydrosugars degraded only under daytime conditions. Among the marker mass fragments of primary biomass burning OA (bbPOA), heavy ones (higher <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>m</mi><mo>/</mo><mi>z</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="63c7f3946b001d4e8415de9c4a1834dd"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-7461-2023-ie00001.svg" width="23pt" height="14pt" src="acp-23-7461-2023-ie00001.png"/></svg:svg></span></span>) were relatively more stable during aging. The biomass burning secondary OA (bbSOA) became more oxidized with continued aging and resembled that of aged atmospheric organic aerosols. The bbSOA formed during daytime oxidation was dominated by acids. Organonitrates were an important product of nighttime reactions in both humid and dry conditions. Our results underline the importance of changes to both the primary and secondary biomass burning aerosols during their atmospheric aging. Heavier fragments from aerosol mass spectrometry seldom used in atmospheric chemistry can be used as more stable tracers of bbPOA and, in combination with the established levoglucosan marker, can provide an indication of the extent of bbPOA aging.</p>https://acp.copernicus.org/articles/23/7461/2023/acp-23-7461-2023.pdf |
spellingShingle | A. Yazdani S. Takahama J. K. Kodros M. Paglione M. Paglione M. Masiol S. Squizzato K. Florou C. Kaltsonoudis S. D. Jorga S. N. Pandis S. N. Pandis A. Nenes A. Nenes Chemical evolution of primary and secondary biomass burning aerosols during daytime and nighttime Atmospheric Chemistry and Physics |
title | Chemical evolution of primary and secondary biomass burning aerosols during daytime and nighttime |
title_full | Chemical evolution of primary and secondary biomass burning aerosols during daytime and nighttime |
title_fullStr | Chemical evolution of primary and secondary biomass burning aerosols during daytime and nighttime |
title_full_unstemmed | Chemical evolution of primary and secondary biomass burning aerosols during daytime and nighttime |
title_short | Chemical evolution of primary and secondary biomass burning aerosols during daytime and nighttime |
title_sort | chemical evolution of primary and secondary biomass burning aerosols during daytime and nighttime |
url | https://acp.copernicus.org/articles/23/7461/2023/acp-23-7461-2023.pdf |
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