Sulphuric acid closure and contribution to nucleation mode particle growth
Sulphuric acid concentrations were measured and calculated based on pseudo steady state model with corresponding measurements of CO, NO<sub>x</sub>, O<sub>3</sub>, SO<sub>2</sub>, methane and non-methane hydrocarbon (NMHC) concentrations as well as solar spectral...
| Main Authors: | , , , , , , , , , , , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2005-01-01
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| Series: | Atmospheric Chemistry and Physics |
| Online Access: | http://www.atmos-chem-phys.net/5/863/2005/acp-5-863-2005.pdf |
| _version_ | 1818561141107851264 |
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| author | M. Boy M. Kulmala T. M. Ruuskanen M. Pihlatie A. Reissell P. P. Aalto P. Keronen M. Dal Maso H. Hellen H. Hakola R. Jansson M. Hanke F. Arnold |
| author_facet | M. Boy M. Kulmala T. M. Ruuskanen M. Pihlatie A. Reissell P. P. Aalto P. Keronen M. Dal Maso H. Hellen H. Hakola R. Jansson M. Hanke F. Arnold |
| author_sort | M. Boy |
| collection | DOAJ |
| description | Sulphuric acid concentrations were measured and calculated based on pseudo steady state model with corresponding measurements of CO, NO<sub>x</sub>, O<sub>3</sub>, SO<sub>2</sub>, methane and non-methane hydrocarbon (NMHC) concentrations as well as solar spectral irradiance and particle number concentrations with size distributions. The measurements were performed as a part of the EU project QUEST (Quantification of Aerosol Nucleation in the European Boundary layer) during an intensive field campaign, which was conducted in Hyytiälä, Finland in March–April 2003. In this paper, the closure between measured and calculated H<sub>2</sub>SO<sub>4</sub> concentrations is investigated. Besides that, also the contribution of sulphuric acid to nucleation mode particle growth rates is studied. Hydroxyl and hydroperoxy radical concentrations were determined using a pseudo steady state box model including photo stationary states. The maximum midday OH concentrations ranged between 4.1×10<sup>5</sup> to 1.8×10<sup>6</sup> molecules cm<sup>-3</sup> and the corresponding values for HO<sub>2</sub> were 1.0×10<sup>7</sup> to 1.5×10<sup>8</sup> molecules cm<sup>-3</sup>. The dominant source term for hydroxyl radicals is the reaction of NO with HO<sub>2</sub> (56%) and the reaction of CO with OH covers around 41% of the sinks. The sulphuric acid source term is the reaction SO<sub>2</sub> with OH and the sink term is condensation of sulphuric acid. The closure between measured and calculated sulphuric acid concentrations is achieved with a high agreement to the measured values. In sensitivity studies, we used different values for the non-methane hydrocarbons, the peroxy radicals and nitrogen dioxide. The best fits between calculated and measured values were found by decreasing the NO<sub>2</sub> concentration when it exceeded values of 1.5 ppb and doubling the non-methane hydrocarbon concentrations. The ratio, standard deviation and correlation coefficient between measured and calculated sulphuric acid concentrations are 0.99, 0.412 and 0.645, respectively. The maximum midday sulphuric acid concentrations varied between 3×10<sup>5</sup> to 1.9×10<sup>7</sup> molecules cm<sup>-3</sup> for the measurements and 3×10<sup>5</sup> to 1.4×10<sup>7</sup> molecules cm<sup>-3</sup> for the calculations, respectively. An average participation of sulphuric acid to the nucleation mode particle growth rates is 8.8%. Classifying the days into two groups – ''polluted'' days with air masses originated over Central Europe or UK, and ''cleaner'' days with air masses originated over the Northern Atlantic or the Polar regions – reflects an equal sulphuric acid contribution to the aerosol growth in both air mass classes. |
| first_indexed | 2024-12-14T00:47:06Z |
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| id | doaj.art-9563d5375e734d30b5541c00ada6d65a |
| institution | Directory Open Access Journal |
| issn | 1680-7316 1680-7324 |
| language | English |
| last_indexed | 2024-12-14T00:47:06Z |
| publishDate | 2005-01-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Atmospheric Chemistry and Physics |
| spelling | doaj.art-9563d5375e734d30b5541c00ada6d65a2022-12-21T23:24:04ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242005-01-0154863878Sulphuric acid closure and contribution to nucleation mode particle growthM. BoyM. KulmalaT. M. RuuskanenM. PihlatieA. ReissellP. P. AaltoP. KeronenM. Dal MasoH. HellenH. HakolaR. JanssonM. HankeF. ArnoldSulphuric acid concentrations were measured and calculated based on pseudo steady state model with corresponding measurements of CO, NO<sub>x</sub>, O<sub>3</sub>, SO<sub>2</sub>, methane and non-methane hydrocarbon (NMHC) concentrations as well as solar spectral irradiance and particle number concentrations with size distributions. The measurements were performed as a part of the EU project QUEST (Quantification of Aerosol Nucleation in the European Boundary layer) during an intensive field campaign, which was conducted in Hyytiälä, Finland in March–April 2003. In this paper, the closure between measured and calculated H<sub>2</sub>SO<sub>4</sub> concentrations is investigated. Besides that, also the contribution of sulphuric acid to nucleation mode particle growth rates is studied. Hydroxyl and hydroperoxy radical concentrations were determined using a pseudo steady state box model including photo stationary states. The maximum midday OH concentrations ranged between 4.1×10<sup>5</sup> to 1.8×10<sup>6</sup> molecules cm<sup>-3</sup> and the corresponding values for HO<sub>2</sub> were 1.0×10<sup>7</sup> to 1.5×10<sup>8</sup> molecules cm<sup>-3</sup>. The dominant source term for hydroxyl radicals is the reaction of NO with HO<sub>2</sub> (56%) and the reaction of CO with OH covers around 41% of the sinks. The sulphuric acid source term is the reaction SO<sub>2</sub> with OH and the sink term is condensation of sulphuric acid. The closure between measured and calculated sulphuric acid concentrations is achieved with a high agreement to the measured values. In sensitivity studies, we used different values for the non-methane hydrocarbons, the peroxy radicals and nitrogen dioxide. The best fits between calculated and measured values were found by decreasing the NO<sub>2</sub> concentration when it exceeded values of 1.5 ppb and doubling the non-methane hydrocarbon concentrations. The ratio, standard deviation and correlation coefficient between measured and calculated sulphuric acid concentrations are 0.99, 0.412 and 0.645, respectively. The maximum midday sulphuric acid concentrations varied between 3×10<sup>5</sup> to 1.9×10<sup>7</sup> molecules cm<sup>-3</sup> for the measurements and 3×10<sup>5</sup> to 1.4×10<sup>7</sup> molecules cm<sup>-3</sup> for the calculations, respectively. An average participation of sulphuric acid to the nucleation mode particle growth rates is 8.8%. Classifying the days into two groups – ''polluted'' days with air masses originated over Central Europe or UK, and ''cleaner'' days with air masses originated over the Northern Atlantic or the Polar regions – reflects an equal sulphuric acid contribution to the aerosol growth in both air mass classes.http://www.atmos-chem-phys.net/5/863/2005/acp-5-863-2005.pdf |
| spellingShingle | M. Boy M. Kulmala T. M. Ruuskanen M. Pihlatie A. Reissell P. P. Aalto P. Keronen M. Dal Maso H. Hellen H. Hakola R. Jansson M. Hanke F. Arnold Sulphuric acid closure and contribution to nucleation mode particle growth Atmospheric Chemistry and Physics |
| title | Sulphuric acid closure and contribution to nucleation mode particle growth |
| title_full | Sulphuric acid closure and contribution to nucleation mode particle growth |
| title_fullStr | Sulphuric acid closure and contribution to nucleation mode particle growth |
| title_full_unstemmed | Sulphuric acid closure and contribution to nucleation mode particle growth |
| title_short | Sulphuric acid closure and contribution to nucleation mode particle growth |
| title_sort | sulphuric acid closure and contribution to nucleation mode particle growth |
| url | http://www.atmos-chem-phys.net/5/863/2005/acp-5-863-2005.pdf |
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