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

被引:415
作者
Jenkin, ME [1 ]
Clemitshaw, KC
机构
[1] AEA Technol Plc, Natl Environm Technol Ctr, Abingdon OX14 3ED, Oxon, England
[2] Univ London Imperial Coll Sci Technol & Med, Ctr Environm Technol, TH Huxley Sch Environm Earth Sci & Engn, Ascot SL5 7PY, Berks, England
关键词
tropospheric oxidation chemistry; secondary pollutants; photochemical processes; planetary boundary layer; ozone; nitrogen oxides; VOCs; organic nitrates; peroxides; secondary organic aerosol;
D O I
10.1016/S1352-2310(99)00478-1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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 in the planetary boundary layer, and may have direct health impacts and/or play wider roles in global atmospheric chemistry. In the present review, a comparatively detailed description of our current understanding of the chemical mechanisms leading to the generation of secondary pollutants in the troposphere is provided, with particular emphasis on chemical processes occurring in the planetary boundary layer. Much of the review is devoted to a discussion 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 secondary pollutants (e.g., organic oxygenates; oxidised organic and inorganic nitrogen compounds), which are often formed in conjunction with O-3, is also described. Some discussion of nighttime chemistry and the formation of secondary organic aerosols (SOA) in tropospheric chemistry is also given, since these are closely linked to the gas-phase photochemical processes. In many cases, the discussion of the relative importance of the various processes 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.
引用
收藏
页码:2499 / 2527
页数:29
相关论文
共 225 条
[1]  
ALLAN BJ, 1997, J ATMOS CHEM, V33, P129
[2]  
ALTSHULLER AP, 1993, J AIR WASTE MANAGE, V43, P1221
[3]   Heterogeneous production of nitrous acid on soot in polluted air masses [J].
Ammann, M ;
Kalberer, M ;
Jost, DT ;
Tobler, L ;
Rössler, E ;
Piguet, D ;
Gäggeler, HW ;
Baltensperger, U .
NATURE, 1998, 395 (6698) :157-160
[4]   PHOTOCHEMICAL OZONE CREATION POTENTIALS - A STUDY OF DIFFERENT CONCEPTS [J].
ANDERSSONSKOLD, Y ;
GRENNFELT, P ;
PLEIJEL, K .
JOURNAL OF THE AIR & WASTE MANAGEMENT ASSOCIATION, 1992, 42 (09) :1152-1158
[5]   A DOAS study on the origin of nitrous acid at urban and non-urban sites [J].
AndresHernandez, MD ;
Notholt, J ;
Hjorth, J ;
Schrems, O .
ATMOSPHERIC ENVIRONMENT, 1996, 30 (02) :175-180
[6]  
ANEJA VP, 1996, ATMOS ENVIRON, V23, P1591
[7]  
[Anonymous], 1986, ENV POL SUS DEV
[8]   KINETICS AND MECHANISMS OF THE GAS-PHASE REACTIONS OF THE NO3 RADICAL WITH ORGANIC-COMPOUNDS [J].
ATKINSON, R .
JOURNAL OF PHYSICAL AND CHEMICAL REFERENCE DATA, 1991, 20 (03) :459-507
[10]   Gas-phase tropospheric chemistry of volatile organic compounds .1. Alkanes and alkenes [J].
Atkinson, R .
JOURNAL OF PHYSICAL AND CHEMICAL REFERENCE DATA, 1997, 26 (02) :215-290