Abstract. Airborne and ground-based measurements of aerosol concentrations, chemicalcomposition, and gas-phase precursors were obtained in three valleys innorthern Utah (USA). The measurements were part of the Utah Winter FineParticulate Study (UWFPS) that took place in January–February 2017. Totalaerosol mass concentrations of PM1 were measured from a Twin Otteraircraft, with an aerosol mass spectrometer (AMS). PM1 concentrationsranged from less than 2µgm−3 during clean periods to over100µgm−3 during the most polluted episodes, consistent withPM2.5 total mass concentrations measured concurrently at groundsites. Across the entire region, increases in total aerosol mass above∼2µgm−3 were associated with increases in theammonium nitrate mass fraction, clearly indicating that the highest aerosolmass loadings in the region were predominantly attributable to an increase inammonium nitrate. The chemical composition was regionally homogenous fortotal aerosol mass concentrations above 17.5µgm−3, with 74±5% (average±standard deviation) ammonium nitrate, 18±3%organic material, 6±3% ammonium sulfate, and 2±2%ammonium chloride. Vertical profiles of aerosol mass and volume in the regionshowed variable concentrations with height in the polluted boundary layer.Higher average mass concentrations were observed within the first few hundredmeters above ground level in all three valleys during pollution episodes. Gas-phase measurements of nitric acid (HNO3) and ammonia (NH3) duringthe pollution episodes revealed that in the Cache and Utah valleys, partitioningof inorganic semi-volatiles to the aerosol phase was usually limited by theamount of gas-phase nitric acid, with NH3 being in excess. The inorganicspecies were compared with the ISORROPIA thermodynamic model. Total inorganicaerosol mass concentrations were calculated for various decreases in totalnitrate and total ammonium. For pollution episodes, our simulations of a50% decrease in total nitrate lead to a 46±3% decrease in totalPM1 mass. A simulated 50% decrease in total ammonium leads to a36±17%µgm−3 decrease in total PM1 mass, over the entirearea of the study. Despite some differences among locations, ourresults showed a higher sensitivity to decreasing nitric acid concentrationsand the importance of ammonia at the lowest total nitrate conditions. In theSalt Lake Valley, both HNO3 and NH3 concentrations controlledaerosol formation.
Abstract. Gas-phase atmospheric concentrations of peroxyacetyl nitrate (PAN),peroxypropionyl nitrate (PPN), and peroxymethacryloyl nitrate (MPAN) weremeasured on the ground using a gas chromatograph electron capture detector(GC-ECD) during the Southern Oxidants and Aerosols Study (SOAS) 2013 campaign(1 June to 15 July 2013) in Centreville, Alabama, in order to studybiosphere–atmosphere interactions. Average levels of PAN, PPN, and MPAN were169, 5, and 9 pptv, respectively, and the sum accounts for an average of16 % of NOy during the daytime (10:00 to 16:00 localtime). Higher concentrations were seen on average in air that came to thesite from the urban NOx sources to the north. PAN levelswere the lowest observed in ground measurements over the past two decades inthe southeastern US. A multiple regression analysis indicates that biogenicvolatile organic compounds (VOCs) account for 66 % of PAN formationduring this study. Comparison of this value with a 0-D model simulation ofperoxyacetyl radical production indicates that at least 50 % of PANformation is due to isoprene oxidation. MPAN has a statistical correlationwith isoprene hydroxynitrates (IN). Organic aerosol mass increases withgas-phase MPAN and IN concentrations, but the mass of organic nitrates inparticles is largely unrelated to MPAN.
more » « less- Award ID(s):
- 1822664
- NSF-PAR ID:
- 10107314
- Date Published:
- Journal Name:
- Atmospheric Chemistry and Physics
- Volume:
- 19
- Issue:
- 3
- ISSN:
- 1680-7324
- Page Range / eLocation ID:
- 1867 to 1880
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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- Free Publicly Accessible Full Text
-
Accepted Manuscript1.0
- Journal Article:
- https://doi.org/10.5194/acp-19-1867-2019
