Organophosphate esters (OPEs) in atmospheric particulate matter in different Brazilian regions

Environ. Sci.: Atmos., 2023, 3,1533-1540
DOI: 10.1039/D3EA00079F, Paper
Open Access Open Access
Priscila Boleta Gonçalves, Joyce Cristale, Amanda Araújo da Silva, Danilo Covaes Nogarotto, Daniela Montanari Migliavacca Osório, Lincoln Lucilio Romualdo, Simone Andréa Pozza
Regional sources and meteorological variables influence the levels of OPEs in PM10 samples from Limeira, Catalão, and Novo Hamburgo. The concentrations found pose no non-carcinogenic risk to human health.
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Spectroscopy of cluster aerosol models: IR and UV spectra of hydrated glyoxylate with and without sea salt

Environ. Sci.: Atmos., 2023, 3,1396-1406
DOI: 10.1039/D3EA00039G, Paper
Open Access Open Access
Creative Commons Licence  This article is licensed under a Creative Commons Attribution 3.0 Unported Licence.
Nina K. Bersenkowitsch, Sarah J. Madlener, Jakob Heller, Christian van der Linde, Milan Ončák, Martin K. Beyer
Tropospheric glyoxylic acid is most likely converted to glyoxylate in sea salt aerosols. We report on the influence of water and salt ions on the structure and photochemistry of glyoxylate.
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Monoethanolamine decay mediated by photolysis of nitrate in atmospheric particles: a brown carbon and organic phase formation pathway

Environ. Sci.: Atmos., 2023, 3,1541-1551
DOI: 10.1039/D3EA00072A, Paper
Open Access Open Access
Creative Commons Licence  This article is licensed under a Creative Commons Attribution 3.0 Unported Licence.
Xiaomeng Tian, Ruifeng Zhang, Bo Wei, Yalin Wang, Yongjie Li, Chak K. Chan
After photolysis, more acidic particles show an increase in pH, while the more neutralized particles show a decrease in pH. NO3 and MEA decay rates are more sensitive to the initial pH than RH. Water-soluble BrC and an organic phase were formed as potential secondary organic aerosols (SOAs).
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Atmospheric oxidation impact on sea spray produced ice nucleating particles

Environ. Sci.: Atmos., 2023, 3,1513-1532
DOI: 10.1039/D3EA00060E, Paper
Open Access Open Access
Paul J. DeMott, Thomas C. J. Hill, Kathryn A. Moore, Russell J. Perkins, Liora E. Mael, Heidi L. Busse, Hansol Lee, Chathuri P. Kaluarachchi, Kathryn J. Mayer, Jonathan S. Sauer, Brock A. Mitts, Alexei V. Tivanski, Vicki H. Grassian, Christopher D. Cappa, Timothy H. Bertram, Kimberly A. Prather
Ice nucleating particles (INPs) in sea spray aerosol (SSA) are important for ice formation in clouds over oceans. We found that SSA INP concentrations during a phytoplankton bloom were degraded with exposure to 3 to 8 days of atmospheric oxidation.
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Assessing formic and acetic acid emissions and chemistry in western U.S. wildfire smoke: implications for atmospheric modeling

Environ. Sci.: Atmos., 2023, Advance Article
DOI: 10.1039/D3EA00098B, Paper
Open Access Open Access
Wade Permar, Catherine Wielgasz, Lixu Jin, Xin Chen, Matthew M. Coggon, Lauren A. Garofalo, Georgios I. Gkatzelis, Damien Ketcherside, Dylan B. Millet, Brett B. Palm, Qiaoyun Peng, Michael A. Robinson, Joel A. Thornton, Patrick Veres, Carsten Warneke, Robert J. Yokelson, Emily V. Fischer, Lu Hu
Rapid production of formic acid in biomass burning smoke is not captured by the Master Chemical Mechanism (MCM) nor simplified GEOS-Chem chemistry, likely due to missing secondary chemical production.
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The driving effects of common atmospheric molecules for formation of clusters: the case of sulfuric acid, nitric acid, hydrochloric acid, ammonia, and dimethylamine

Environ. Sci.: Atmos., 2023, Advance Article
DOI: 10.1039/D3EA00118K, Paper
Open Access Open Access
Olivia M. Longsworth, Conor J. Bready, Macie S. Joines, George C. Shields
Secondary aerosols form from gas-phase molecules that create prenucleation complexes, which grow to form aerosols. Understanding how secondary aerosols form in the atmosphere is essential for a better understanding of global warming.
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A national crowdsourced network of low-cost fine particulate matter and aerosol optical depth monitors: results from the 2021 wildfire season in the United States

Environ. Sci.: Atmos., 2023, 3,1563-1575
DOI: 10.1039/D3EA00086A, Paper
Open Access Open Access
Creative Commons Licence  This article is licensed under a Creative Commons Attribution 3.0 Unported Licence.
Eric A. Wendt, Bonne Ford, Michael Cheeseman, Zoey Rosen, Jeffrey R. Pierce, Shantanu H. Jathar, Christian L'Orange, Casey Quinn, Marilee Long, John Mehaffy, Daniel D. Miller-Lionberg, David H. Hagan, John Volckens
A novel instrument designed for crowdsourced data collection on air quality and aerosol optical depth.
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VOC emissions by fresh and old asphalt pavements at service temperatures: impacts on urban air quality

Environ. Sci.: Atmos., 2023, Advance Article
DOI: 10.1039/D3EA00034F, Paper
Open Access Open Access
J. Lasne, A. Lostier, M. N. Romanias, S. Vassaux, D. Lesueur, V. Gaudion, M. Jamar, R. G. Derwent, S. Dusanter, T. Salameh
VOC emissions from asphalt pavements at service temperature contribute significantly to SOA formation in urban areas.
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Molecular and physical composition of tar balls in wildfire smoke: an investigation with complementary ionisation methods and 15-Tesla FT-ICR mass spectrometry

Environ. Sci.: Atmos., 2023, 3,1552-1562
DOI: 10.1039/D3EA00085K, Paper
Open Access Open Access
Amna Ijaz, William Kew, Zezhen Cheng, Susan Mathai, Nurun Nahar Lata, Libor Kovarik, Simeon Schum, Swarup China, Lynn R. Mazzoleni
Laser desorption ionisation, coupled with ultrahigh-resolution mass spectrometry, provides an apt reflection of the physical properties of tar balls in wildfire smoke.
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Acoustic levitation with polarising optical microscopy (AL-POM): water uptake in a nanostructured atmospheric aerosol proxy

Environ. Sci.: Atmos., 2023, Advance Article
DOI: 10.1039/D3EA00083D, Paper
Open Access Open Access
Creative Commons Licence  This article is licensed under a Creative Commons Attribution 3.0 Unported Licence.
Adam Milsom, Adam M. Squires, Christopher Brasnett, William N. Sharratt, Annela M. Seddon, Christian Pfrang
We present acoustic levitation combined with polarising optical microscopy (AL-POM). Fatty acid aerosols were probed and a model fit revealed a ca. 5–6 orders of magnitude difference in water diffusion coefficient upon a phase transition between optically birefringent and non-birefringent phases.
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