Chapter 10 100 Years of Progress in Gas-Phase Atmospheric Chemistry Research
CHAPTER 10 WALLINGTON ET AL. 10.1 Chapter 10 100 Years of Progress in Gas-Phase Atmospheric Chemistry Research T. J. WALLINGTON Research and Advanced Engineering, Ford Motor Company, Dearborn, Michigan J. H. SEINFELD California Institute of Technology, Pasadena, California J. R. BARKER Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, Michigan ABSTRACT Remarkable progress has occurred over the last 100 years in our understanding of atmospheric chemical composition, stratospheric and tropospheric chemistry, urban air pollution, acid rain, and the formation of airborne particles from gas-phase chemistry. Much of this progress was associated with the developing un- derstanding of the formation and role of ozone and of the oxides of nitrogen, NO and NO2, in the stratosphere and troposphere. The chemistry of the stratosphere, emerging from the pioneering work of Chapman in 1931, was followed by the discovery of catalytic ozone cycles, ozone destruction by chlorofluorocarbons, and the polar ozone holes, work honored by the 1995 Nobel Prize in Chemistry awarded to Crutzen, Rowland, and Molina. Foundations for the modern understanding of tropospheric chemistry were laid in the 1950s and 1960s, stimulated by the eye-stinging smog in Los Angeles. The importance of the hydroxyl (OH) radical and its relationship to the oxides of nitrogen (NO and NO2) emerged. The chemical processes leading to acid rain were elucidated. The atmosphere contains an immense number of gas-phase organic compounds, a result of emissions from plants and animals, natural and anthropogenic combustion processes, emissions from oceans, and from the atmospheric oxidation of organics emitted into the atmosphere.
[Show full text]