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

<p>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 At...

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Published in:Atmospheric Chemistry and Physics
Main Authors: J. M. Mattila, P. Brophy, J. Kirkland, S. Hall, K. Ullmann, E. V. Fischer, S. Brown, E. McDuffie, A. Tevlin, D. K. Farmer
Format: Article
Language:English
Published: Copernicus Publications 2018-08-01
Online Access:https://www.atmos-chem-phys.net/18/12315/2018/acp-18-12315-2018.pdf
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author J. M. Mattila
P. Brophy
J. Kirkland
S. Hall
K. Ullmann
E. V. Fischer
S. Brown
S. Brown
E. McDuffie
E. McDuffie
E. McDuffie
A. Tevlin
D. K. Farmer
author_facet J. M. Mattila
P. Brophy
J. Kirkland
S. Hall
K. Ullmann
E. V. Fischer
S. Brown
S. Brown
E. McDuffie
E. McDuffie
E. McDuffie
A. Tevlin
D. K. Farmer
author_sort J. M. Mattila
collection DOAJ
container_title Atmospheric Chemistry and Physics
description <p>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 HNO<sub>3</sub>, HNCO, formic, propionic, butyric, valeric, and pyruvic acid. Vertical profiles taken on the 300&thinsp;m tower demonstrate net surface-level emissions of alkanoic acids, but net surface deposition of HNO<sub>3</sub> and pyruvic acid. The surface-level alkanoic acid source persists through both day and night, and is thus not solely photochemical. Reactions between O<sub>3</sub> 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 HNO<sub>3</sub> 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.</p>
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spelling doaj-art-6d640583e79549bdb67445fdf2d64e7e2025-08-19T21:00:11ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242018-08-0118123151232710.5194/acp-18-12315-2018Tropospheric sources and sinks of gas-phase acids in the Colorado Front RangeJ. M. Mattila0P. Brophy1J. Kirkland2S. Hall3K. Ullmann4E. V. Fischer5S. Brown6S. Brown7E. McDuffie8E. McDuffie9E. McDuffie10A. Tevlin11D. K. Farmer12Department of Chemistry, Colorado State University, Fort Collins, CO, USADepartment of Chemistry, Colorado State University, Fort Collins, CO, USADepartment of Chemistry, Colorado State University, Fort Collins, CO, USAAtmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, CO, USAAtmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, CO, USADepartment of Atmospheric Science, Colorado State University, Fort Collins, CO, USANOAA Earth System Research Laboratory, Chemical Sciences Division, Boulder, CO, USADepartment of Chemistry and Biochemistry, University of Colorado Boulder, Boulder, CO, USANOAA Earth System Research Laboratory, Chemical Sciences Division, Boulder, CO, USADepartment of Chemistry and Biochemistry, University of Colorado Boulder, Boulder, CO, USACooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USADepartment of Chemistry, University of Toronto, Toronto, ON, CanadaDepartment of Chemistry, Colorado State University, Fort Collins, CO, USA<p>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 HNO<sub>3</sub>, HNCO, formic, propionic, butyric, valeric, and pyruvic acid. Vertical profiles taken on the 300&thinsp;m tower demonstrate net surface-level emissions of alkanoic acids, but net surface deposition of HNO<sub>3</sub> and pyruvic acid. The surface-level alkanoic acid source persists through both day and night, and is thus not solely photochemical. Reactions between O<sub>3</sub> 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 HNO<sub>3</sub> 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.</p>https://www.atmos-chem-phys.net/18/12315/2018/acp-18-12315-2018.pdf
spellingShingle J. M. Mattila
P. Brophy
J. Kirkland
S. Hall
K. Ullmann
E. V. Fischer
S. Brown
S. Brown
E. McDuffie
E. McDuffie
E. McDuffie
A. Tevlin
D. K. Farmer
Tropospheric sources and sinks of gas-phase acids in the Colorado Front Range
title Tropospheric sources and sinks of gas-phase acids in the Colorado Front Range
title_full Tropospheric sources and sinks of gas-phase acids in the Colorado Front Range
title_fullStr Tropospheric sources and sinks of gas-phase acids in the Colorado Front Range
title_full_unstemmed Tropospheric sources and sinks of gas-phase acids in the Colorado Front Range
title_short Tropospheric sources and sinks of gas-phase acids in the Colorado Front Range
title_sort tropospheric sources and sinks of gas phase acids in the colorado front range
url https://www.atmos-chem-phys.net/18/12315/2018/acp-18-12315-2018.pdf
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