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DOI | 10.5194/acp-19-13053-2019 |
Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season | |
Glicker H.S.; Lawler M.J.; Ortega J.; De Sá S.S.; Martin S.T.; Artaxo P.; Vega Bustillos O.; De Souza R.; Tota J.; Carlton A.; Smith J.N. | |
发表日期 | 2019 |
ISSN | 16807316 |
起始页码 | 13053 |
结束页码 | 13066 |
卷号 | 19期号:20 |
英文摘要 | 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 chemical ionization 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 epoxydiol (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 ultrafine 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. © 2019 Author(s). |
语种 | 英语 |
scopus关键词 | aerosol composition; chemical composition; formation mechanism; metropolitan area; particle size; volatile organic compound; wet season; Amazonas [Brazil]; Amazonia; Brazil; Manaus |
来源期刊 | Atmospheric Chemistry and Physics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/144077 |
作者单位 | Department of Chemistry, University of California, Irvine, Irvine, CA 92697, United States; School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138, United States; Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, United States; Institute of Physics, University of São Paulo, Rua do Matão 1371, São Paulo, SP, 05508-090, Brazil; Chemistry and Environment Center, Instituto de Pesquisas Energéticas e Nucleares, São Paulo, SP, 05508-000, Brazil; Meteorology Department, Universidade do Estado do Amazonas, Manaus, AM, 69050-020, Brazil; Institute of Engineering and Geoscience, Universidade Federal do Oeste do Pará, Santarém, PA, 68035-110, Brazil |
推荐引用方式 GB/T 7714 | Glicker H.S.,Lawler M.J.,Ortega J.,et al. Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season[J],2019,19(20). |
APA | Glicker H.S..,Lawler M.J..,Ortega J..,De Sá S.S..,Martin S.T..,...&Smith J.N..(2019).Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season.Atmospheric Chemistry and Physics,19(20). |
MLA | Glicker H.S.,et al."Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season".Atmospheric Chemistry and Physics 19.20(2019). |
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