A kinetic model for ozone uptake by solutions and aqueous particles containing I and Br, including seawater and sea-salt aerosol

The heterogeneous interactions of gaseous ozone (O 3 ) with seawater and with sea-salt aerosols are known to generate volatile halogen species, which, in turn, lead to further destruction of O 3 . Here, a kinetic model for the interaction of ozone (O 3 ) with Br − and I − solutions and aqueous parti...

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Bibliographic Details
Published in:Physical chemistry chemical physics : PCCP 2019, Vol.21 (36), p.19835-19856
Main Authors: Moreno, Carolina, Baeza-Romero, María Teresa
Format: Article
Language:English
Subjects:
Aerosols
Halides
Ozone
Saline solutions
Seawater
Surface reactions
Troposphere
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Summary:The heterogeneous interactions of gaseous ozone (O 3 ) with seawater and with sea-salt aerosols are known to generate volatile halogen species, which, in turn, lead to further destruction of O 3 . Here, a kinetic model for the interaction of ozone (O 3 ) with Br − and I − solutions and aqueous particles has been proposed that satisfactorily explains previous literature studies about this process. Apart from the aqueous-phase reactions X − + O 3 (X = I, Br), the interaction also involves the surface reactions X − + O 3 that occur via O 3 adsorption on the aqueous surface. In single salt solutions and aerosols, the partial order in ozone and the total order of the surface reactions are one, but the apparent total order is second order because the number of ozone sites where reaction can occur is equal to the surficial concentration of X − ([X − ] surf ). In the presence of Cl − , the surface reactions are enhanced by a factor equal to , where and . Therefore, we have inferred that Cl − acts as a catalyst in the surface reactions X − + O 3 . The model has been applied to estimate ozone uptake by the reaction with these halides in/on seawater and in/on sea-salt aerosol, where it has been concluded that the Cl − -catalyzed surface reaction is important relative to total ozone uptake and should therefore be considered to model Y/YO (Y = I, Br, Cl) levels in the troposphere. The heterogeneous interactions of gaseous ozone (O 3 ) with seawater and with sea-salt aerosols are known to generate volatile halogen species, which, in turn, lead to further destruction of O 3 . Cl − acts as a catalyst in the surface reactions X − + O 3 .
ISSN:1463-9076
1463-9084
DOI:10.1039/c9cp03430g