Ozone and other secondary photochemical pollutants: chemical processes governing their formation in the planetary boundary layer

Citation
Me. Jenkin et Kc. Clemitshaw, Ozone and other secondary photochemical pollutants: chemical processes governing their formation in the planetary boundary layer, ATMOS ENVIR, 34(16), 2000, pp. 2499-2527
Citations number
224
Categorie Soggetti
Environment/Ecology,"Earth Sciences
Journal title
ATMOSPHERIC ENVIRONMENT
ISSN journal
13522310 → ACNP
Volume
34
Issue
16
Year of publication
2000
Pages
2499 - 2527
Database
ISI
SICI code
1352-2310(2000)34:16<2499:OAOSPP>2.0.ZU;2-L
Abstract
The chemical processing of pollutants emitted into the atmosphere leads to a variety of oxidised products, which are commonly referred to as secondary pollutants. Such pollutants are often formed on local or regional scales i n the planetary boundary layer, and may have direct health impacts and/or p lay wider roles in global atmospheric chemistry. In the present review, a c omparatively detailed description of our current understanding of the chemi cal mechanisms leading to the generation of secondary pollutants in the tro posphere is provided, with particular emphasis on chemical processes occurr ing in the planetary boundary layer. Much of the review is devoted to a dis cussion of the gas-phase photochemical transformations of nitrogen oxides ( NOx) and volatile organic compounds (VOCs), and their role in the formation of ozone (O-3) The chemistry producing a variety of other oxidants and sec ondary pollutants (e.g., organic oxygenates; oxidised organic and inorganic nitrogen compounds), which are often formed in conjunction with O-3, is al so described. Some discussion of nighttime chemistry and the formation of s econdary organic aerosols (SOA) in tropospheric chemistry is also given, si nce these are closely linked to the gas-phase photochemical processes. In m any cases, the discussion of the relative importance of the various process es is illustrated by observational data, with emphasis generally placed on conditions appropriate to the UK and northwest continental Europe. (C) 2000 Elsevier Science Ltd. All rights reserved.