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Gas‐particle partitioning of primary organic aerosol emissions: 3. Biomass burning
Author(s) -
May Andrew A.,
Levin Ezra J. T.,
Hennigan Christopher J.,
Riipinen Ilona,
Lee Taehyoung,
Collett Jeffrey L.,
Jimenez Jose L.,
Kreidenweis Sonia M.,
Robinson Allen L.
Publication year - 2013
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/jgrd.50828
Subject(s) - aerosol , volatility (finance) , dilution , plume , combustion , chemistry , atmospheric sciences , vaporization , particle (ecology) , environmental chemistry , environmental science , meteorology , thermodynamics , physics , organic chemistry , financial economics , economics , geology , oceanography
Atmospheric organic aerosol concentrations depend in part on the gas‐particle partitioning of primary organic aerosol (POA) emissions. Consequently, heating and dilution were used to investigate the volatility of biomass‐burning smoke particles from combustion of common North American trees/shrubs/grasses during the third Fire Lab at Missoula Experiment. Fifty to eighty percent of the mass of biomass‐burning POA evaporated when isothermally diluted from plume‐ (~1000 µg m −3 ) to ambient‐like concentrations (~10 µg m −3 ), while roughly 80% of the POA evaporated upon heating to 100°C in a thermodenuder with a residence time of ~14 sec. Therefore, the majority of the POA emissions were semivolatile. Thermodenuder measurements performed at three different residence times indicated that there were not substantial mass transfer limitations to evaporation (i.e., the mass accommodation coefficient appears to be between 0.1 and 1). An evaporation kinetics model was used to derive volatility distributions and enthalpies of vaporization from the thermodenuder data. A single volatility distribution can be used to represent the measured gas‐particle partitioning from the entire set of experiments, including different fuels, organic aerosol concentrations, and thermodenuder residence times. This distribution, derived from the thermodenuder measurements, also predicts the dilution‐driven changes in gas‐particle partitioning. This volatility distribution and associated emission factors for each fuel studied can be used to update emission inventories and to simulate the gas‐particle partitioning of biomass‐burning POA emissions in chemical transport models.