examples of secondary aerosols


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PDF 1 Primary and Secondary Sources of Atmospheric Aerosol

Atmospheric aerosols are suspensions of any substance existing in the solid and/or liquid phase in the atmosphere (except pure water) under normal condi-

  • What is secondary aerosol formation?

    Secondary Organic Aerosol (SOA) is formed– by definition –when low volatility oxidation products of volatile organic compounds (VOCs) deposit onto existing particles or form new particles.
    SOA accounts for a major fraction of the global atmospheric aerosol burden.

  • What are the 5 examples of aerosols?

    The five most common classifications of aerosols are dust, fume, mist, smoke, and fog.
    Generally, dust describes large, solid aerosols.
    Fumes are small, liquid aerosols.

  • What are secondary sources of aerosols in the atmosphere?

    Secondary aerosol particles are produced in the atmosphere from precursor gases by condensation of vapours on pre-existing particles or by nucleation of new particles.
    A considerable fraction of the mass of secondary aerosols is formed through cloud processing (Ervens et al. 2011).

  • Sea salt, dust, and volcanic ash are three common types of aerosols. (Photograph by Katherine Mann.) The bulk of aerosols—about 90 percent by mass—have natural origins.
    Volcanoes, for example, eject huge columns of ash into the air, as well as sulfur dioxide and other gases, yielding sulfates.

Sea spray, mineral dust, smoke, and volcanic ash are all primary aerosols. Secondary aerosols are aerosols which were emitted in another form (e.g. gases), then become aerosol particles after going through chemical reactions in the atmosphere, such as sulfate aerosols from volcanoes or industrial emissions.
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