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ATR-FTIR characterization of organic functional groups and inorganic ions in ambient aerosols at a rural site
Authors:Charity Coury  Ann M Dillner
Institution:1. School of Environmental and Chemical Engineering, Shanghai University, Shanghai 200444, China;2. Guangzhou Hexin Analytical Instrument Company Limited, Guangzhou 510530, China;3. State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Science, Beijing 100012, China;4. Atmospheric Environment Institute of Safety and Pollution Control, Jinan University, Guangdong 510632, China;1. Laborelec, Rodestraat 125, 1630 Linkebeek, Belgium;2. Karlsruhe Institute of Technology (KIT), Institut für Technische Thermodynamik und Kältetechnik, Engler-Bunte-Ring 21, 76131 Karlsruhe, Germany;3. TNO, Leeghwaterstraat 46, Delft 2628CA, The Netherlands
Abstract:An Attenuated Total Reflectance-Fourier Transform Infrared (ATR-FTIR) spectroscopic method was used to measure organic functional groups and inorganic ions at Tonto National Monument (TNM), an Interagency Monitoring of Protected Visual Environments (IMPROVE) sampling site in a rural area near Phoenix, Arizona. Functional groups and ions from common aerosol compound classes such as aliphatic and aromatic CH, methylene, methyl, aldehydes/ketones, carboxylic acids, ammonium sulfate and nitrate as well as functional groups from difficult to measure compound classes such as esters/lactones, acid anhydrides, carbohydrate hydroxyl and ethers, amino acids, and amines were quantified. On average, ~33% of the PM1.0 mass was composed of organic aerosol. The average (standard deviation) composition of the organic aerosol at TNM was 34% (6%) biogenic functional groups, 21% (5%) oxygenated functional groups, 28% (7%) aliphatic hydrocarbon functional groups (aliphatic CH, methylene and methyl) and 17% (1%) aromatic hydrocarbon functional groups. Compositional analysis, functional group correlations, and back trajectories were used to identify three types of events with source signatures: primary biogenic-influenced, urban-influenced, and regional background. The biogenic-influenced event had high concentrations of amino acids and carbohydrate hydroxyl and ether, as well as aliphatic CH and aromatic CH functional groups and qualitatively high levels of silicate. The urban-influenced events had back trajectories traveling directly from the Phoenix area and high concentrations of hydrocarbons, oxygenated functional groups, and inorganic ions. This aerosol characterization suggests that both primary emissions in Phoenix and secondary formation of aerosols from Phoenix emissions had a major impact on the aerosol composition and concentration at TNM. The regional background source had low concentrations of all functional groups, but had higher concentrations of biogenic functional groups than the urban source.
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