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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2013-07-01
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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: γ<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 γ<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: γ<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 γ<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 |
work_keys_str_mv |
AT ybedjanian uptakeofhosub2subradicalsonarizonatestdust AT mnromanias uptakeofhosub2subradicalsonarizonatestdust AT aelzein uptakeofhosub2subradicalsonarizonatestdust |
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