Diel cycle impacts on the chemical and light absorption properties of organic carbon aerosol from wildfires in the western United States
Organic aerosol (OA) emissions from biomass burning have been the subject of intense research in recent years, involving a combination of field campaigns and laboratory studies. These efforts have aimed at improving our limited understanding of the diverse processes and pathways involved in the atmo...
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Published in | Atmospheric chemistry and physics Vol. 21; no. 15; pp. 11843 - 11856 |
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Main Authors | , , , , , , , , |
Format | Journal Article |
Language | English |
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Katlenburg-Lindau
Copernicus GmbH
09.08.2021
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Abstract | Organic aerosol (OA) emissions from biomass burning have
been the subject of intense research in recent years, involving a
combination of field campaigns and laboratory studies. These efforts have
aimed at improving our limited understanding of the diverse processes and
pathways involved in the atmospheric processing and evolution of OA
properties, culminating in their accurate parameterizations in climate and
chemical transport models. To bring closure between laboratory and field
studies, wildfire plumes in the western United States were sampled and
characterized for their chemical and optical properties during the
ground-based segment of the 2019 Fire Influence on Regional to Global
Environments and Air Quality (FIREX-AQ) field campaign. Using a
custom-developed multiwavelength integrated photoacoustic-nephelometer
spectrometer in conjunction with a suite of instruments, including an
oxidation flow reactor equipped to generate hydroxyl (OH⚫) or
nitrate (NO3⚫) radicals to mimic daytime or nighttime
oxidative aging processes, we investigated the effects of multiple
equivalent hours of OH⚫ or NO3⚫ exposure on
the chemical composition and mass absorption cross-sections (MAC(λ)) at 488 and 561 nm of OA emitted from wildfires in Arizona and Oregon. We
found that OH⚫ exposure induced a slight initial increase in
absorption corresponding to short timescales; however, at longer timescales, the wavelength-dependent MAC(λ) decreased by a factor of
0.72 ± 0.08, consistent with previous laboratory studies and reports
of photobleaching. On the other hand, NO3⚫ exposure increased
MAC(λ) by a factor of up to 1.69 ± 0.38. We also noted some
sensitivity of aerosol aging to different fire conditions between Arizona
and Oregon. The MAC(λ) enhancement following NO3⚫ exposure was found to correlate with an enhancement in CHO1N and
CHOgt1N ion families measured by an Aerodyne aerosol mass spectrometer. |
---|---|
AbstractList | Organic aerosol (OA) emissions from biomass burning have been the subject of intense research in recent years, involving a combination of field campaigns and laboratory studies. These efforts have aimed at improving our limited understanding of the diverse processes and pathways involved in the atmospheric processing and evolution of OA properties, culminating in their accurate parameterizations in climate and chemical transport models. To bring closure between laboratory and field studies, wildfire plumes in the western United States were sampled and characterized for their chemical and optical properties during the ground-based segment of the 2019 Fire Influence on Regional to Global Environments and Air Quality (FIREX-AQ) field campaign. Using a custom-developed multiwavelength integrated photoacoustic-nephelometer spectrometer in conjunction with a suite of instruments, including an oxidation flow reactor equipped to generate hydroxyl (OH⚫) or nitrate (NO 3 ⚫) radicals to mimic daytime or nighttime oxidative aging processes, we investigated the effects of multiple equivalent hours of OH⚫ or NO 3 ⚫ exposure on the chemical composition and mass absorption cross-sections (MAC( λ )) at 488 and 561 nm of OA emitted from wildfires in Arizona and Oregon. We found that OH⚫ exposure induced a slight initial increase in absorption corresponding to short timescales; however, at longer timescales, the wavelength-dependent MAC( λ ) decreased by a factor of 0.72 ± 0.08, consistent with previous laboratory studies and reports of photobleaching. On the other hand, NO 3 ⚫ exposure increased MAC( λ ) by a factor of up to 1.69 ± 0.38. We also noted some sensitivity of aerosol aging to different fire conditions between Arizona and Oregon. The MAC( λ ) enhancement following NO 3 ⚫ exposure was found to correlate with an enhancement in CHO 1 N and CHO gt1 N ion families measured by an Aerodyne aerosol mass spectrometer. Organic aerosol (OA) emissions from biomass burning have been the subject of intense research in recent years, involving a combination of field campaigns and laboratory studies. These efforts have aimed at improving our limited understanding of the diverse processes and pathways involved in the atmospheric processing and evolution of OA properties, culminating in their accurate parameterizations in climate and chemical transport models. To bring closure between laboratory and field studies, wildfire plumes in the western United States were sampled and characterized for their chemical and optical properties during the ground-based segment of the 2019 Fire Influence on Regional to Global Environments and Air Quality (FIREX-AQ) field campaign. Using a custom-developed multiwavelength integrated photoacoustic-nephelometer spectrometer in conjunction with a suite of instruments, including an oxidation flow reactor equipped to generate hydroxyl (OHâ«) or nitrate (NO.sub.3 â«) radicals to mimic daytime or nighttime oxidative aging processes, we investigated the effects of multiple equivalent hours of OHâ« or NO.sub.3 â« exposure on the chemical composition and mass absorption cross-sections (MAC(λ)) at 488 and 561 nm of OA emitted from wildfires in Arizona and Oregon. We found that OHâ« exposure induced a slight initial increase in absorption corresponding to short timescales; however, at longer timescales, the wavelength-dependent MAC(λ) decreased by a factor of 0.72 ± 0.08, consistent with previous laboratory studies and reports of photobleaching. On the other hand, NO.sub.3 â« exposure increased MAC(λ) by a factor of up to 1.69 ± 0.38. We also noted some sensitivity of aerosol aging to different fire conditions between Arizona and Oregon. The MAC(λ) enhancement following NO.sub.3 â« exposure was found to correlate with an enhancement in CHO.sub.1 N and CHO.sub.gt1 N ion families measured by an Aerodyne aerosol mass spectrometer. Organic aerosol (OA) emissions from biomass burning have been the subject of intense research in recent years, involving a combination of field campaigns and laboratory studies. These efforts have aimed at improving our limited understanding of the diverse processes and pathways involved in the atmospheric processing and evolution of OA properties, culminating in their accurate parameterizations in climate and chemical transport models. To bring closure between laboratory and field studies, wildfire plumes in the western United States were sampled and characterized for their chemical and optical properties during the ground-based segment of the 2019 Fire Influence on Regional to Global Environments and Air Quality (FIREX-AQ) field campaign. Using a custom-developed multiwavelength integrated photoacoustic-nephelometer spectrometer in conjunction with a suite of instruments, including an oxidation flow reactor equipped to generate hydroxyl (OH⚫) or nitrate (NO3⚫) radicals to mimic daytime or nighttime oxidative aging processes, we investigated the effects of multiple equivalent hours of OH⚫ or NO3⚫ exposure on the chemical composition and mass absorption cross-sections (MAC(λ)) at 488 and 561 nm of OA emitted from wildfires in Arizona and Oregon. We found that OH⚫ exposure induced a slight initial increase in absorption corresponding to short timescales; however, at longer timescales, the wavelength-dependent MAC(λ) decreased by a factor of 0.72 ± 0.08, consistent with previous laboratory studies and reports of photobleaching. On the other hand, NO3⚫ exposure increased MAC(λ) by a factor of up to 1.69 ± 0.38. We also noted some sensitivity of aerosol aging to different fire conditions between Arizona and Oregon. The MAC(λ) enhancement following NO3⚫ exposure was found to correlate with an enhancement in CHO1N and CHOgt1N ion families measured by an Aerodyne aerosol mass spectrometer. Organic aerosol (OA) emissions from biomass burning have been the subject of intense research in recent years, involving a combination of field campaigns and laboratory studies. These efforts have aimed at improving our limited understanding of the diverse processes and pathways involved in the atmospheric processing and evolution of OA properties, culminating in their accurate parameterizations in climate and chemical transport models. To bring closure between laboratory and field studies, wildfire plumes in the western United States were sampled and characterized for their chemical and optical properties during the ground-based segment of the 2019 Fire Influence on Regional to Global Environments and Air Quality (FIREX-AQ) field campaign. Using a custom-developed multiwavelength integrated photoacoustic-nephelometer spectrometer in conjunction with a suite of instruments, including an oxidation flow reactor equipped to generate hydroxyl (OH•) or nitrate (NO3•) radicals to mimic daytime or nighttime oxidative aging processes, we investigated the effects of multiple equivalent hours of OH• or NO3• exposure on the chemical composition and mass absorption cross-sections (MAC(λ)) at 488 and 561 nm of OA emitted from wildfires in Arizona and Oregon. We found that OH• exposure induced a slight initial increase in absorption corresponding to short timescales; however, at longer timescales, the wavelength-dependent MAC(λ) decreased by a factor of 0.72 ± 0.08, consistent with previous laboratory studies and reports of photobleaching. On the other hand, NO3• exposure increased MAC(λ) by a factor of up to 1.69 ± 0.38. We also noted some sensitivity of aerosol aging to different fire conditions between Arizona and Oregon. The MAC(λ) enhancement following NO3• exposure was found to correlate with an enhancement in CHO1N and CHOgt1N ion families measured by an Aerodyne aerosol mass spectrometer. Organic aerosol (OA) emissions from biomass burning have been the subject of intense research in recent years, involving a combination of field campaigns and laboratory studies. These efforts have aimed at improving our limited understanding of the diverse processes and pathways involved in the atmospheric processing and evolution of OA properties, culminating in their accurate parameterizations in climate and chemical transport models. To bring closure between laboratory and field studies, wildfire plumes in the western United States were sampled and characterized for their chemical and optical properties during the ground-based segment of the 2019 Fire Influence on Regional to Global Environments and Air Quality (FIREX-AQ) field campaign. Using a custom-developed multiwavelength integrated photoacoustic-nephelometer spectrometer in conjunction with a suite of instruments, including an oxidation flow reactor equipped to generate hydroxyl (OH⚫) or nitrate (NO3⚫) radicals to mimic daytime or nighttime oxidative aging processes, we investigated the effects of multiple equivalent hours of OH⚫ or NO3⚫ exposure on the chemical composition and mass absorption cross-sections (MAC(λ)) at 488 and 561 nm of OA emitted from wildfires in Arizona and Oregon. We found that OH⚫ exposure induced a slight initial increase in absorption corresponding to short timescales; however, at longer timescales, the wavelength-dependent MAC(λ) decreased by a factor of 0.72 ± 0.08, consistent with previous laboratory studies and reports of photobleaching. On the other hand, NO3⚫ exposure increased MAC(λ) by a factor of up to 1.69 ± 0.38. We also noted some sensitivity of aerosol aging to different fire conditions between Arizona and Oregon. The MAC(λ) enhancement following NO3⚫ exposure was found to correlate with an enhancement in CHO1N and CHOgt1N ion families measured by an Aerodyne aerosol mass spectrometer. |
Audience | Academic |
Author | Shetty, Nishit J. Fortner, Edward Majluf, Francesca Liu, Pai Daube, Conner Sumlin, Benjamin Lambe, Andrew Herndon, Scott Chakrabarty, Rajan K. |
Author_xml | – sequence: 1 givenname: Benjamin orcidid: 0000-0003-2909-7494 surname: Sumlin fullname: Sumlin, Benjamin – sequence: 2 givenname: Edward surname: Fortner fullname: Fortner, Edward – sequence: 3 givenname: Andrew orcidid: 0000-0003-3031-701X surname: Lambe fullname: Lambe, Andrew – sequence: 4 givenname: Nishit J. surname: Shetty fullname: Shetty, Nishit J. – sequence: 5 givenname: Conner orcidid: 0000-0001-8296-0272 surname: Daube fullname: Daube, Conner – sequence: 6 givenname: Pai surname: Liu fullname: Liu, Pai – sequence: 7 givenname: Francesca surname: Majluf fullname: Majluf, Francesca – sequence: 8 givenname: Scott orcidid: 0000-0002-7348-8225 surname: Herndon fullname: Herndon, Scott – sequence: 9 givenname: Rajan K. orcidid: 0000-0001-5753-9937 surname: Chakrabarty fullname: Chakrabarty, Rajan K. |
BackLink | https://www.osti.gov/biblio/1812411$$D View this record in Osti.gov |
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Cites_doi | 10.1073/pnas.1804353115 10.2172/57153 10.1063/1.555887 10.1029/1998JD100054 10.1080/02786826.2012.663948 10.1038/nchem.948 10.5194/acp-9-1263-2009 10.5194/amt-4-445-2011 10.1021/acs.analchem.8b02641 10.1029/2007JD009699 10.1364/OL.28.001007 10.1021/acs.est.9b05641 10.1021/es401043j 10.5194/acp-9-163-2009 10.1063/1.1322585 10.5194/acp-10-6363-2010 10.5194/acp-17-5331-2017 10.1029/1999GL010935 10.1016/j.jqsrt.2017.12.009 10.1021/cr5006167 10.1021/es0019169 10.1364/E2.2011.EThC2 10.1021/acs.est.0c06838 10.1021/es00142a006 10.1021/acs.est.8b00093 10.1364/AO.42.003726 10.1029/2007GL029979 10.1029/2006JD007340 10.1002/mas.20115 10.1063/1.1581355 10.1029/2003JD004169 10.1021/acs.est.7b05864 10.1021/acsearthspacechem.0c00117 10.1364/AO.50.000A74 10.5194/acp-20-13417-2020 10.1175/BAMS-D-14-00110.1 10.1080/02786826.2018.1531107 10.1021/acs.estlett.7b00393 10.5194/amt-11-1741-2018 10.5194/amt-13-2397-2020 10.5194/acp-19-2899-2019 10.1021/acs.est.0c04310 10.1139/X07-143 10.5194/acp-11-12049-2011 10.1080/02786826.2020.1726867 10.1016/S1352-2310(98)00361-6 10.1080/027868200410840 10.1073/pnas.1404727111 10.5194/amt-11-6577-2018 10.1080/02786820802389251 10.5194/acp-13-11551-2013 |
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CorporateAuthor | Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Atmospheric Radiation Measurement (ARM) Data Center |
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Snippet | Organic aerosol (OA) emissions from biomass burning have
been the subject of intense research in recent years, involving a
combination of field campaigns and... Organic aerosol (OA) emissions from biomass burning have been the subject of intense research in recent years, involving a combination of field campaigns and... |
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StartPage | 11843 |
SubjectTerms | Absorption Absorption cross sections Aerosol absorption Aerosols Ageing Aging Air quality Analysis Atmospheric models Biomass Biomass burning Burning Carbon aerosols Chemical composition Chemical transport Climate change Climate models Electromagnetic absorption ENVIRONMENTAL SCIENCES Experiments Exposure Fire plumes Fires Forest & brush fires Information systems Instruments Laboratories Light Light absorption Mass spectrometry Nephelometers Optical properties Organic carbon Oxidation Photobleaching Plumes Wavelength Wildfires |
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Title | Diel cycle impacts on the chemical and light absorption properties of organic carbon aerosol from wildfires in the western United States |
URI | https://www.proquest.com/docview/2559396909 https://www.osti.gov/biblio/1812411 https://doaj.org/article/1347d608d2c84f6f9b2d82729de470dc |
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