Processes controlling the concentration of hydroperoxides at Jungfraujoch Observatory, Switzerland

An automated, ground-based instrument was used to measure gas-phase hydroperoxides at the Jungfraujoch High Altitude Research Station as part of the Free Tropospheric EXperiment (FREETEX) during February/March 2003. A nebulising reflux concentrator sampled ambient air twice hourly, prior to on-site...

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Main Authors: S. J. Walker, M. J. Evans, A. V. Jackson, M. Steinbacher, C. Zellweger, J. B. McQuaid
Format: Article
Language:English
Published: Copernicus Publications 2006-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/6/5525/2006/acp-6-5525-2006.pdf
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author S. J. Walker
M. J. Evans
A. V. Jackson
M. Steinbacher
C. Zellweger
J. B. McQuaid
author_facet S. J. Walker
M. J. Evans
A. V. Jackson
M. Steinbacher
C. Zellweger
J. B. McQuaid
author_sort S. J. Walker
collection DOAJ
description An automated, ground-based instrument was used to measure gas-phase hydroperoxides at the Jungfraujoch High Altitude Research Station as part of the Free Tropospheric EXperiment (FREETEX) during February/March 2003. A nebulising reflux concentrator sampled ambient air twice hourly, prior to on-site analysis by HPLC speciation, coupled with post-column peroxidase derivatisation and fluorescence detection. Hydrogen peroxide (H<sub>2</sub>O<sub>2</sub>) concentrations reached up to 1330 pptv over the 13-day period with a mean of 183&plusmn;233 pptv (&plusmn; one standard deviation). Methyl hydroperoxide (CH<sub>3</sub>OOH) reached up to 379 pptv with a mean of 51&plusmn;55 pptv. No other organic hydroperoxides were detected. The lack of an explicit diurnal cycle suggests that hydroperoxide concentrations are chiefly influenced by transport processes rather than local photochemistry at this mountainous site. There was some evidence that elevated concentrations of H<sub>2</sub>O<sub>2</sub> existed in air-masses originating from the south-west, suggesting higher concentrations of HO<sub>x</sub> due to more active photochemistry. Air which had been recently polluted exhibited low H<sub>2</sub>O<sub>2</sub> concentration due to a combination of suppression of HO<sub>2</sub> by NO<sub>x</sub> and deposition. The concentrations of H<sub>2</sub>O<sub>2</sub> sampled here are consistent with previous box modelling studies of hydroperoxides, except in periods influenced by the boundary layer, where agreement required a depositional sink.
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spelling doaj.art-ff2e021f0fcf43d1984a115cea30250c2022-12-22T02:27:08ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242006-01-0161255255536Processes controlling the concentration of hydroperoxides at Jungfraujoch Observatory, SwitzerlandS. J. WalkerM. J. EvansA. V. JacksonM. SteinbacherC. ZellwegerJ. B. McQuaidAn automated, ground-based instrument was used to measure gas-phase hydroperoxides at the Jungfraujoch High Altitude Research Station as part of the Free Tropospheric EXperiment (FREETEX) during February/March 2003. A nebulising reflux concentrator sampled ambient air twice hourly, prior to on-site analysis by HPLC speciation, coupled with post-column peroxidase derivatisation and fluorescence detection. Hydrogen peroxide (H<sub>2</sub>O<sub>2</sub>) concentrations reached up to 1330 pptv over the 13-day period with a mean of 183&plusmn;233 pptv (&plusmn; one standard deviation). Methyl hydroperoxide (CH<sub>3</sub>OOH) reached up to 379 pptv with a mean of 51&plusmn;55 pptv. No other organic hydroperoxides were detected. The lack of an explicit diurnal cycle suggests that hydroperoxide concentrations are chiefly influenced by transport processes rather than local photochemistry at this mountainous site. There was some evidence that elevated concentrations of H<sub>2</sub>O<sub>2</sub> existed in air-masses originating from the south-west, suggesting higher concentrations of HO<sub>x</sub> due to more active photochemistry. Air which had been recently polluted exhibited low H<sub>2</sub>O<sub>2</sub> concentration due to a combination of suppression of HO<sub>2</sub> by NO<sub>x</sub> and deposition. The concentrations of H<sub>2</sub>O<sub>2</sub> sampled here are consistent with previous box modelling studies of hydroperoxides, except in periods influenced by the boundary layer, where agreement required a depositional sink.http://www.atmos-chem-phys.net/6/5525/2006/acp-6-5525-2006.pdf
spellingShingle S. J. Walker
M. J. Evans
A. V. Jackson
M. Steinbacher
C. Zellweger
J. B. McQuaid
Processes controlling the concentration of hydroperoxides at Jungfraujoch Observatory, Switzerland
Atmospheric Chemistry and Physics
title Processes controlling the concentration of hydroperoxides at Jungfraujoch Observatory, Switzerland
title_full Processes controlling the concentration of hydroperoxides at Jungfraujoch Observatory, Switzerland
title_fullStr Processes controlling the concentration of hydroperoxides at Jungfraujoch Observatory, Switzerland
title_full_unstemmed Processes controlling the concentration of hydroperoxides at Jungfraujoch Observatory, Switzerland
title_short Processes controlling the concentration of hydroperoxides at Jungfraujoch Observatory, Switzerland
title_sort processes controlling the concentration of hydroperoxides at jungfraujoch observatory switzerland
url http://www.atmos-chem-phys.net/6/5525/2006/acp-6-5525-2006.pdf
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