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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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> mixtures under atmospheric conditions. The estimated upper limits for the uptake coefficients of NO<sub>2</sub> and the reactive uptake coefficients NO<sub>2 </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> mixtures under atmospheric conditions. The estimated upper limits for the uptake coefficients of NO<sub>2</sub> and the reactive uptake coefficients NO<sub>2 </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 |
work_keys_str_mv |
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