Tropospheric sources and sinks of gas-phase acids in the Colorado Front Range

We measured organic and inorganic gas-phase acids in the Front Range of Colorado to better understand their tropospheric sources and sinks using a high-resolution time-of-flight chemical ionization mass spectrometer. Measurements were conducted from 4 to 13 August 2014 at the Boulder Atmospheric Obs...

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Veröffentlicht in:Atmospheric chemistry and physics 2018-08, Vol.18 (16), p.12315-12327
Hauptverfasser: Mattila, James M, Brophy, Patrick, Kirkland, Jeffrey, Hall, Samuel, Ullmann, Kirk, Fischer, Emily V, Brown, Steve, McDuffie, Erin, Tevlin, Alex, Farmer, Delphine K
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Sprache:eng
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Zusammenfassung:We measured organic and inorganic gas-phase acids in the Front Range of Colorado to better understand their tropospheric sources and sinks using a high-resolution time-of-flight chemical ionization mass spectrometer. Measurements were conducted from 4 to 13 August 2014 at the Boulder Atmospheric Observatory during the Front Range Air Pollution and Photochemistry Éxperiment. Diurnal increases in mixing ratios are consistent with photochemical sources of HNO3, HNCO, formic, propionic, butyric, valeric, and pyruvic acid. Vertical profiles taken on the 300 m tower demonstrate net surface-level emissions of alkanoic acids, but net surface deposition of HNO3 and pyruvic acid. The surface-level alkanoic acid source persists through both day and night, and is thus not solely photochemical. Reactions between O3 and organic surfaces may contribute to the surface-level alkanoic acid source. Nearby traffic emissions and agricultural activity are a primary source of propionic, butyric, and valeric acids, and likely contribute photochemical precursors to HNO3 and HNCO. The combined diel and vertical profiles of the alkanoic acids and HNCO are inconsistent with dry deposition and photochemical losses being the only sinks, suggesting additional loss mechanisms.
ISSN:1680-7324
1680-7316
1680-7324
DOI:10.5194/acp-18-12315-2018