Halogen production from aqueous tropospheric particles.
Box model studies have been performed to study the role of aqueous phase chemistry with regard to halogen activation for marine and urban clouds and the marine aerosol as well. Different chemical pathways leading to halogen activation in diluted cloud droplets and highly concentrated sea salt aerosol particles are investigated. The concentration of halides in cloud droplets is significantly smaller than in sea-salt particles, and hence different reaction sequences control the overall chemical conversions. In diluted droplets radical chemistry involving OH, NO(3), Cl/Cl(2)(-)/ClOH(-), and Br/Br(2)(-)/BrOH(-) gains in importance and pH independent pathways lead to the release of halogens from the particle phase whereas the chemistry in aerosol particles with high electrolyte concentrations is controlled by non-radical reactions at high ionic strengths and relatively low pH values. For the simulation of halogen activation in tropospheric clouds and aqueous aerosol particles in different environments a halogen module was developed including both gas and aqueous phase processes of halogen containing species. This module is coupled to a base mechanism consisting of RACM (Regional Atmospheric Chemistry Mechanism) and the Chemical Aqueous Phase Radical Mechanism CAPRAM 2.4 (MODAC-mechanism). Phase exchange is described by the resistance model by Chemistry of Multiphase Atmospheric Systems, NATO ASI Series, 1986. It can be shown that under cloud conditions the bromine atom is mainly produced by OH initiated reactions, i.e. its concentration maximum is reached at noon. In contrast, the concentration level of chlorine atoms is linked to NO(3) radical chemistry leading to a smaller amplitude between day and night time concentrations. The contribution of radical processes to halogen atom formation in the particle phase is evident, e.g. by halogen atoms which undergo direct phase transfer. Furthermore, the application of the multiphase model for initial concentrations for sea-salt aerosols shows that the particle phase can act as a main source of halogen containing molecules (Cl(2), BrCl, Br(2)) which are photolysed in the gas phase to yield halogen atoms (about 70% of all Cl sources and more than 99% for Br).
Herrmann
H
H
Institut für Troposphärenforschung, Permoserstrasse 15, 04318 Leipzig, Germany. hermann@tropos.de
Majdik
Z
Z
Ervens
B
B
Weise
D
D
D000336:Aerosols / Q000737:chemistry; D000393:Air Pollutants / Q000737:chemistry*; D001272:Atmosphere / Q000737:chemistry*; D005609:Free Radicals / Q000737:chemistry; D006219:Halogens / Q000032:analysis / Q000737:chemistry*; D006878:Hydroxides / Q000737:chemistry; D008685:Meteorological Concepts; D008956:Models, Chemical; D009566:Nitrates / Q000737:chemistry; D010316:Particle Size; D010777:Photochemistry; D012965:Sodium Chloride / Q000032:analysis / Q000737:chemistry
D000336:Aerosols; D000393:Air Pollutants; D005609:Free Radicals; D006219:Halogens; D006878:Hydroxides; D009566:Nitrates; D012965:Sodium Chloride