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Heterogeneous conversion of NO2 on secondary organic aerosol surfaces: A possible source of nitrous acid (HONO) in the atmosphere?

Item

Title (Dublin Core)

Heterogeneous conversion of NO2 on secondary organic aerosol surfaces: A possible source of nitrous acid (HONO) in the atmosphere?

Description (Dublin Core)

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> -&gt; 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 &lt;10<sup>13</sup> cm<sup>-2</sup> geometrical surface and &lt;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>-&gt; 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.

Creator (Dublin Core)

Bröske, R.
Kleffmann, J.
Wiesen, P.

Date (Dublin Core)

2018-06-29

Type (Dublin Core)

Text

Format (Dublin Core)

application/pdf

Identifier (Dublin Core)

10.5194/acp-3-469-2003
https://acp.copernicus.org/articles/3/469/2003/

Source (Dublin Core)

eISSN: 1680-7324

Language (Dublin Core)

eng
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