Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season
Abstract
Central Amazonia serves as an ideal location to study atmospheric particle formation, since it often represents nearly natural, pre-industrial conditions but can also experience periods of anthropogenic influence due to the presence of emissions from large metropolitan areas like Manaus, Brazil. Ultrafine (sub-100 nm diameter) particles are often observed in this region, although new particle formation events seldom occur near the ground despite being readily observed in other forested regions with similar emissions of volatile organic compounds (VOCs). This study focuses on identifying the chemical composition of ultrafine particles as a means of determining the chemical species and mechanisms that may be responsible for new particle formation and growth in the region. These measurements were performed during the wet season as part of the Observations and Modeling of the Green Ocean Amazon (GoAmazon2014/5) field campaign at a site located 70 km southwest of Manaus. A thermal desorption chemicalionization mass spectrometer (TDCIMS) characterized the most abundant compounds detected in ultrafine particles. Two time periods representing distinct influences on aerosol composition, which we label as “anthropogenic” and “background” periods, were studied as part of a larger 10 d period of analysis. Higher particle number concentrations were measured during the anthropogenic period, andmore »
- Authors:
-
- Univ. of California, Irvine, CA (United States). Dept. of Chemistry
- Harvard Univ., Cambridge, MA (United States). School of Engineering and Applied Sciences
- Harvard Univ., Cambridge, MA (United States). School of Engineering and Applied Sciences and Dept. of Earth and Planetary Sciences
- Univ. of Sao Paulo (Brazil). Inst. of Physics
- Instituto de Pesquisas Energéticas e Nucleares, Sao Paulo (Brazil). Chemistry and Environment Center
- Universidade do Estado do Amazonas (Brazil). Meteorology Dept.
- Universidade Federal do Oeste do Pará (Brazil). Inst. of Engineering and Geoscience
- Publication Date:
- Research Org.:
- Harvard Univ., Cambridge, MA (United States); Univ. of California, Irvine, CA (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC)
- OSTI Identifier:
- 1802213
- Grant/Contract Number:
- SC0011115; SC0011122
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Atmospheric Chemistry and Physics (Online)
- Additional Journal Information:
- Journal Name: Atmospheric Chemistry and Physics (Online); Journal Volume: 19; Journal Issue: 20; Journal ID: ISSN 1680-7324
- Publisher:
- Copernicus Publications, EGU
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; 37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY
Citation Formats
Glicker, Hayley S., Lawler, Michael J., Ortega, John, de Sá, Suzane S., Martin, Scot T., Artaxo, Paulo, Vega Bustillos, Oscar, de Souza, Rodrigo, Tota, Julio, Carlton, Annmarie, and Smith, James N. Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season. United States: N. p., 2019.
Web. doi:10.5194/acp-19-13053-2019.
Glicker, Hayley S., Lawler, Michael J., Ortega, John, de Sá, Suzane S., Martin, Scot T., Artaxo, Paulo, Vega Bustillos, Oscar, de Souza, Rodrigo, Tota, Julio, Carlton, Annmarie, & Smith, James N. Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season. United States. https://doi.org/10.5194/acp-19-13053-2019
Glicker, Hayley S., Lawler, Michael J., Ortega, John, de Sá, Suzane S., Martin, Scot T., Artaxo, Paulo, Vega Bustillos, Oscar, de Souza, Rodrigo, Tota, Julio, Carlton, Annmarie, and Smith, James N. Wed .
"Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season". United States. https://doi.org/10.5194/acp-19-13053-2019. https://www.osti.gov/servlets/purl/1802213.
@article{osti_1802213,
title = {Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season},
author = {Glicker, Hayley S. and Lawler, Michael J. and Ortega, John and de Sá, Suzane S. and Martin, Scot T. and Artaxo, Paulo and Vega Bustillos, Oscar and de Souza, Rodrigo and Tota, Julio and Carlton, Annmarie and Smith, James N.},
abstractNote = {Central Amazonia serves as an ideal location to study atmospheric particle formation, since it often represents nearly natural, pre-industrial conditions but can also experience periods of anthropogenic influence due to the presence of emissions from large metropolitan areas like Manaus, Brazil. Ultrafine (sub-100 nm diameter) particles are often observed in this region, although new particle formation events seldom occur near the ground despite being readily observed in other forested regions with similar emissions of volatile organic compounds (VOCs). This study focuses on identifying the chemical composition of ultrafine particles as a means of determining the chemical species and mechanisms that may be responsible for new particle formation and growth in the region. These measurements were performed during the wet season as part of the Observations and Modeling of the Green Ocean Amazon (GoAmazon2014/5) field campaign at a site located 70 km southwest of Manaus. A thermal desorption chemicalionization mass spectrometer (TDCIMS) characterized the most abundant compounds detected in ultrafine particles. Two time periods representing distinct influences on aerosol composition, which we label as “anthropogenic” and “background” periods, were studied as part of a larger 10 d period of analysis. Higher particle number concentrations were measured during the anthropogenic period, and modeled back-trajectory frequencies indicate transport of emissions from the Manaus metropolitan area. During the background period there were much lower number concentrations, and back-trajectory frequencies showed that air masses arrived at the site predominantly from the forested regions to the north and northeast. TDCIMS-measured constituents also show distinct differences between the two observational periods. Although bisulfate was detected in particles throughout the 10 d period, the anthropogenic period had higher levels of particulate bisulfate overall. Ammonium and trimethyl ammonium were positively correlated with bisulfate. The background period had distinct diurnal patterns of particulate cyanate and acetate, while oxalate remained relatively constant during the 10 d period. 3-Methylfuran, a thermal decomposition product of a particulate-phase isoprene epoxy diol(IEPOX), was the dominant species measured in the positive-ion mode. Principal component analysis (PCA) was performed on the TDCIMS-measured ion abundance and aerosol mass spectrometer (AMS) mass concentration data. Two different hierarchical clusters representing unique influences arise: one comprising ultrafine particulate acetate, hydrogen oxalate, cyanate, trimethyl ammonium and 3-methylfuran and another made up of ultra fine particulate bisulfate, chloride, ammonium and potassium. A third cluster separated AMS-measured species from the two TDCIMS-derived clusters, indicating different sources or processes in ultrafine aerosol particle formation compared to larger submicron-sized particles.},
doi = {10.5194/acp-19-13053-2019},
journal = {Atmospheric Chemistry and Physics (Online)},
number = 20,
volume = 19,
place = {United States},
year = {Wed Oct 23 00:00:00 EDT 2019},
month = {Wed Oct 23 00:00:00 EDT 2019}
}
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Works referencing / citing this record:
Mixing states of Amazon basin aerosol particles transported over long distances using transmission electron microscopy
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