Uptake of HO<sub>2</sub> radicals on Arizona Test Dust

The interaction of HO<sub>2</sub> radicals with solid films of Arizona Test Dust (ATD) was studied using a low-pressure flow reactor (1–9 Torr) combined with a modulated molecular beam mass spectrometer for monitoring of the gaseous species involved. The reactive uptake coefficient of HO...

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Main Authors: Y. Bedjanian, M. N. Romanias, A. El Zein
Format: Article
Language:English
Published: Copernicus Publications 2013-07-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/6461/2013/acp-13-6461-2013.pdf
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spelling doaj-f1162ed882894cc8a9ee89fcbbafdfa92020-11-24T20:57:09ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-07-0113136461647110.5194/acp-13-6461-2013Uptake of HO<sub>2</sub> radicals on Arizona Test DustY. BedjanianM. N. RomaniasA. El ZeinThe interaction of HO<sub>2</sub> radicals with solid films of Arizona Test Dust (ATD) was studied using a low-pressure flow reactor (1–9 Torr) combined with a modulated molecular beam mass spectrometer for monitoring of the gaseous species involved. The reactive uptake coefficient of HO<sub>2</sub> was measured from the kinetics of HO<sub>2</sub> consumption on Pyrex rods coated with ATD as a function of HO<sub>2</sub> concentration ((0.35–3.30) × 10<sup>12</sup> molecule cm<sup>−3</sup>), relative humidity (RH = 0.02–94%), temperature (<i>T</i> = 275–320 K) and UV irradiance intensity (<i>J</i><sub>NO<sub>2</sub></sub> = 0–0.012 s<sup>−1</sup>). The initial uptake coefficient was found to be independent of concentration of HO<sub>2</sub>, temperature and irradiation conditions, and to decrease with increasing relative humidity: &gamma;<sub>0</sub> = 1.2/(18.7 + RH<sub>1.1</sub>) (with 30% estimated conservative uncertainty). The uptake coefficient was calculated using geometric surface area and should be considered as an upper limit of &gamma;<sub>0</sub>. An upper limit of 5% was found for the gaseous H<sub>2</sub>O<sub>2</sub>-forming pathway of the HO<sub>2</sub> reaction with ATD surface. The results of the measurements indicate that HO<sub>2</sub> loss on dust aerosol may be a non-negligible sink for HO<sub>x</sub> species in the troposphere with the effect depending on specific local conditions.http://www.atmos-chem-phys.net/13/6461/2013/acp-13-6461-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Y. Bedjanian
M. N. Romanias
A. El Zein
spellingShingle Y. Bedjanian
M. N. Romanias
A. El Zein
Uptake of HO<sub>2</sub> radicals on Arizona Test Dust
Atmospheric Chemistry and Physics
author_facet Y. Bedjanian
M. N. Romanias
A. El Zein
author_sort Y. Bedjanian
title Uptake of HO<sub>2</sub> radicals on Arizona Test Dust
title_short Uptake of HO<sub>2</sub> radicals on Arizona Test Dust
title_full Uptake of HO<sub>2</sub> radicals on Arizona Test Dust
title_fullStr Uptake of HO<sub>2</sub> radicals on Arizona Test Dust
title_full_unstemmed Uptake of HO<sub>2</sub> radicals on Arizona Test Dust
title_sort uptake of ho<sub>2</sub> radicals on arizona test dust
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2013-07-01
description The interaction of HO<sub>2</sub> radicals with solid films of Arizona Test Dust (ATD) was studied using a low-pressure flow reactor (1–9 Torr) combined with a modulated molecular beam mass spectrometer for monitoring of the gaseous species involved. The reactive uptake coefficient of HO<sub>2</sub> was measured from the kinetics of HO<sub>2</sub> consumption on Pyrex rods coated with ATD as a function of HO<sub>2</sub> concentration ((0.35–3.30) × 10<sup>12</sup> molecule cm<sup>−3</sup>), relative humidity (RH = 0.02–94%), temperature (<i>T</i> = 275–320 K) and UV irradiance intensity (<i>J</i><sub>NO<sub>2</sub></sub> = 0–0.012 s<sup>−1</sup>). The initial uptake coefficient was found to be independent of concentration of HO<sub>2</sub>, temperature and irradiation conditions, and to decrease with increasing relative humidity: &gamma;<sub>0</sub> = 1.2/(18.7 + RH<sub>1.1</sub>) (with 30% estimated conservative uncertainty). The uptake coefficient was calculated using geometric surface area and should be considered as an upper limit of &gamma;<sub>0</sub>. An upper limit of 5% was found for the gaseous H<sub>2</sub>O<sub>2</sub>-forming pathway of the HO<sub>2</sub> reaction with ATD surface. The results of the measurements indicate that HO<sub>2</sub> loss on dust aerosol may be a non-negligible sink for HO<sub>x</sub> species in the troposphere with the effect depending on specific local conditions.
url http://www.atmos-chem-phys.net/13/6461/2013/acp-13-6461-2013.pdf
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AT mnromanias uptakeofhosub2subradicalsonarizonatestdust
AT aelzein uptakeofhosub2subradicalsonarizonatestdust
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