Heterogeneous conversion of NO<sub>2</sub> on secondary organic aerosol surfaces: A possible source of nitrous acid (HONO) in the atmosphere?

The heterogeneous conversion of NO<sub>2</sub> on different secondary organic aerosols (SOA) was investigated with the focus on a possible formation of nitrous acid (HONO). In one set of experiments different organic aerosols were produced in the reactions of O<sub>3</sub>...

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Main Authors: R. Bröske, J. Kleffmann, P. Wiesen
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/3/469/2003/acp-3-469-2003.pdf
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spelling doaj-3840d0928d11457cb4801bfac076a50f2020-11-24T23:57:20ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242003-01-0133469474Heterogeneous conversion of NO<sub>2</sub> on secondary organic aerosol surfaces: A possible source of nitrous acid (HONO) in the atmosphere?R. BröskeJ. KleffmannP. WiesenThe heterogeneous conversion of NO<sub>2</sub> on different secondary organic aerosols (SOA) was investigated with the focus on a possible formation of nitrous acid (HONO). In one set of experiments different organic aerosols were produced in the reactions of O<sub>3</sub> with alpha-pinene, limonene or catechol and OH radicals with toluene or limonene, respectively. The aerosols were sampled on filters and exposed to humidified NO<sub>2</sub>&nbsp; mixtures under atmospheric conditions. The estimated upper limits for the uptake coefficients of NO<sub>2</sub>&nbsp; and the reactive uptake coefficients NO<sub>2&nbsp;</sub> -> HONO are in the range of 10<sup>-6 </sup>and 10<sup>-7</sup>, respectively. The integrated HONO formation for 1 h reaction time was <10<sup>13</sup> cm<sup>-2</sup> geometrical surface and <10<sup>17</sup> g<sup>-1</sup> particle mass. In a second set of experiments the conversion of NO<sub>2</sub> into HONO in the presence of organic particles was carried out in an aerosol flow tube under atmospheric conditions. In this case the aerosols were produced in the reaction of O<sub>3</sub> with beta-pinene, limonene or catechol, respectively. The upper limits for the reactive uptake coefficients NO<sub>2 </sub>-> HONO were in the range of 7 x 10<sup>-7 </sup>- 9 x 10<sup>-6</sup>. The results from the present study show that heterogeneous formation of nitrous acid on secondary organic aerosols (SOA) is unimportant for the atmosphere.http://www.atmos-chem-phys.net/3/469/2003/acp-3-469-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. Bröske
J. Kleffmann
P. Wiesen
spellingShingle R. Bröske
J. Kleffmann
P. Wiesen
Heterogeneous conversion of NO<sub>2</sub> on secondary organic aerosol surfaces: A possible source of nitrous acid (HONO) in the atmosphere?
Atmospheric Chemistry and Physics
author_facet R. Bröske
J. Kleffmann
P. Wiesen
author_sort R. Bröske
title Heterogeneous conversion of NO<sub>2</sub> on secondary organic aerosol surfaces: A possible source of nitrous acid (HONO) in the atmosphere?
title_short Heterogeneous conversion of NO<sub>2</sub> on secondary organic aerosol surfaces: A possible source of nitrous acid (HONO) in the atmosphere?
title_full Heterogeneous conversion of NO<sub>2</sub> on secondary organic aerosol surfaces: A possible source of nitrous acid (HONO) in the atmosphere?
title_fullStr Heterogeneous conversion of NO<sub>2</sub> on secondary organic aerosol surfaces: A possible source of nitrous acid (HONO) in the atmosphere?
title_full_unstemmed Heterogeneous conversion of NO<sub>2</sub> on secondary organic aerosol surfaces: A possible source of nitrous acid (HONO) in the atmosphere?
title_sort heterogeneous conversion of no<sub>2</sub> on secondary organic aerosol surfaces: a possible source of nitrous acid (hono) in the atmosphere?
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2003-01-01
description The heterogeneous conversion of NO<sub>2</sub> on different secondary organic aerosols (SOA) was investigated with the focus on a possible formation of nitrous acid (HONO). In one set of experiments different organic aerosols were produced in the reactions of O<sub>3</sub> with alpha-pinene, limonene or catechol and OH radicals with toluene or limonene, respectively. The aerosols were sampled on filters and exposed to humidified NO<sub>2</sub>&nbsp; mixtures under atmospheric conditions. The estimated upper limits for the uptake coefficients of NO<sub>2</sub>&nbsp; and the reactive uptake coefficients NO<sub>2&nbsp;</sub> -> HONO are in the range of 10<sup>-6 </sup>and 10<sup>-7</sup>, respectively. The integrated HONO formation for 1 h reaction time was <10<sup>13</sup> cm<sup>-2</sup> geometrical surface and <10<sup>17</sup> g<sup>-1</sup> particle mass. In a second set of experiments the conversion of NO<sub>2</sub> into HONO in the presence of organic particles was carried out in an aerosol flow tube under atmospheric conditions. In this case the aerosols were produced in the reaction of O<sub>3</sub> with beta-pinene, limonene or catechol, respectively. The upper limits for the reactive uptake coefficients NO<sub>2 </sub>-> HONO were in the range of 7 x 10<sup>-7 </sup>- 9 x 10<sup>-6</sup>. The results from the present study show that heterogeneous formation of nitrous acid on secondary organic aerosols (SOA) is unimportant for the atmosphere.
url http://www.atmos-chem-phys.net/3/469/2003/acp-3-469-2003.pdf
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