Fine Aerosol Acidity and Water during Summer in the Eastern North Atlantic
Abstract
Aerosol pH governs many important atmospheric processes that occur in the marine boundary layer, including regulating halogen and sulfur chemistries, and nutrient fertilization of surface ocean waters. In this study, we investigated the acidity of PM1 over the eastern North Atlantic during the Aerosol and Cloud Experiments in Eastern North Atlantic (ACE-ENA) aircraft campaign. The ISORROPIA-II thermodynamic model was used to predict PM1 pH and water. We first investigated the sensitivities of PM1 pH and water predictions to gas-phase NH3 and HNO3 concentrations. Our sensitivity analysis indicated that even though NH3 and HNO3 were present at very low concentrations in the eastern North Atlantic during the campaign, PM1 pH calculations can still be sensitive to NH3 concentrations. Specifically, NH3 was needed to constrain the pH of populations of PM1 that had low mass concentrations of NH4+ and non-volatile cations (NVCs). We next assumed that gas-phase NH3 and HNO3 concentrations during the campaign were 0.15 and 0.09 µg m-3, respectively, based on previous measurements conducted in the eastern North Atlantic. Using the assumption that PM1 were internally mixed (i.e., bulk PM1), we determined that PM1 pH ranged from 0.3–8.6, with a mean pH of 5.0 ± 2.3. The pH depended on both $$H^{+}_{air}$$ and $$W_{i}$$. $$H^{+}_{air}$$ was controlled primarily by the NVCs/SO42- molar ratio, while Wi was controlled by the SO42 mass concentration and RH. Changes in pH with altitude were driven primarily by changes in SO42-. Since aerosols in marine atmospheres are rarely internally mixed, the scenario where non-sea salt species and sea-salt species were present in two separate aerosol modes in the PM1 (i.e., completely externally mixed) was also considered. Smaller pH values were predicted for the aerosol mode comprised only of non-sea salt species compared to the bulk PM1 (difference of around 1 unit on average). This was due to the exclusion of sea-salt species (especially hygroscopic alkaline NVCs) in this aerosol mode, which led to increases in $$H^{+}_{air}$$ values and decreases in $$W_{i}$$ values. This result demonstrated that assumptions of aerosol mixing states can impact aerosol pH predictions substantially, which will have important implications for evaluating the nature and magnitude of pH-dependent atmospheric processes that occur in the marine boundary layer.
- Authors:
- Publication Date:
- Research Org.:
- Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States); City Univ. of Hong Kong, Kowloon (Hong Kong); Washington Univ., St. Louis, MO (United States); Colorado State Univ., Fort Collins, CO (United States); Georgia Institute of Technology, Atlanta, GA (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC), Biological and Environmental Research (BER)
- OSTI Identifier:
- 1813078
- Alternate Identifier(s):
- OSTI ID: 1813546; OSTI ID: 1837832
- Grant/Contract Number:
- DOE 333890; SC0020259; 333890
- Resource Type:
- Published Article
- Journal Name:
- Atmosphere (Basel)
- Additional Journal Information:
- Journal Name: Atmosphere (Basel) Journal Volume: 12 Journal Issue: 8; Journal ID: ISSN 2073-4433
- Publisher:
- MDPI AG
- Country of Publication:
- Switzerland
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; aerosol water; aerosol pH; aqueous phase; remote marine boundary layer; non-volatile cations
Citation Formats
Nah, Theodora, Yang, Junwei, Wang, Jian, Sullivan, Amy P., and Weber, Rodney J. Fine Aerosol Acidity and Water during Summer in the Eastern North Atlantic. Switzerland: N. p., 2021.
Web. doi:10.3390/atmos12081040.
Nah, Theodora, Yang, Junwei, Wang, Jian, Sullivan, Amy P., & Weber, Rodney J. Fine Aerosol Acidity and Water during Summer in the Eastern North Atlantic. Switzerland. https://doi.org/10.3390/atmos12081040
Nah, Theodora, Yang, Junwei, Wang, Jian, Sullivan, Amy P., and Weber, Rodney J. Fri .
"Fine Aerosol Acidity and Water during Summer in the Eastern North Atlantic". Switzerland. https://doi.org/10.3390/atmos12081040.
@article{osti_1813078,
title = {Fine Aerosol Acidity and Water during Summer in the Eastern North Atlantic},
author = {Nah, Theodora and Yang, Junwei and Wang, Jian and Sullivan, Amy P. and Weber, Rodney J.},
abstractNote = {Aerosol pH governs many important atmospheric processes that occur in the marine boundary layer, including regulating halogen and sulfur chemistries, and nutrient fertilization of surface ocean waters. In this study, we investigated the acidity of PM1 over the eastern North Atlantic during the Aerosol and Cloud Experiments in Eastern North Atlantic (ACE-ENA) aircraft campaign. The ISORROPIA-II thermodynamic model was used to predict PM1 pH and water. We first investigated the sensitivities of PM1 pH and water predictions to gas-phase NH3 and HNO3 concentrations. Our sensitivity analysis indicated that even though NH3 and HNO3 were present at very low concentrations in the eastern North Atlantic during the campaign, PM1 pH calculations can still be sensitive to NH3 concentrations. Specifically, NH3 was needed to constrain the pH of populations of PM1 that had low mass concentrations of NH4+ and non-volatile cations (NVCs). We next assumed that gas-phase NH3 and HNO3 concentrations during the campaign were 0.15 and 0.09 µg m-3, respectively, based on previous measurements conducted in the eastern North Atlantic. Using the assumption that PM1 were internally mixed (i.e., bulk PM1), we determined that PM1 pH ranged from 0.3–8.6, with a mean pH of 5.0 ± 2.3. The pH depended on both $H^{+}_{air}$ and $W_{i}$. $H^{+}_{air}$ was controlled primarily by the NVCs/SO42- molar ratio, while Wi was controlled by the SO42 mass concentration and RH. Changes in pH with altitude were driven primarily by changes in SO42-. Since aerosols in marine atmospheres are rarely internally mixed, the scenario where non-sea salt species and sea-salt species were present in two separate aerosol modes in the PM1 (i.e., completely externally mixed) was also considered. Smaller pH values were predicted for the aerosol mode comprised only of non-sea salt species compared to the bulk PM1 (difference of around 1 unit on average). This was due to the exclusion of sea-salt species (especially hygroscopic alkaline NVCs) in this aerosol mode, which led to increases in $H^{+}_{air}$ values and decreases in $W_{i}$ values. This result demonstrated that assumptions of aerosol mixing states can impact aerosol pH predictions substantially, which will have important implications for evaluating the nature and magnitude of pH-dependent atmospheric processes that occur in the marine boundary layer.},
doi = {10.3390/atmos12081040},
journal = {Atmosphere (Basel)},
number = 8,
volume = 12,
place = {Switzerland},
year = {Fri Aug 13 00:00:00 EDT 2021},
month = {Fri Aug 13 00:00:00 EDT 2021}
}
https://doi.org/10.3390/atmos12081040
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