Environ. Sci. Technol., 36 (11), 2345 -2353, 2002. 10.1021/es011381z S0013-936X(01)01381-5
Web Release Date: May 2, 2002

Copyright © 2002 American Chemical Society

Effects of Meteorological Conditions on Aerosol Composition and Mixing State in Bakersfield, CA

Jeffrey R. Whiteaker, David T. Suess, and Kimberly A. Prather*

Department of Chemistry, University of California, Riverside, Riverside, California 92521, and Department of Chemistry and Biochemistry, University of California, San Diego, 9500 Gilman Drive, La Jolla, California 92093-0314

Received for review October 23, 2001

Revised manuscript received March 14, 2002

Accepted March 20, 2002

Abstract:

Particle and meteorological instrumentation were used to characterize ambient atmospheric conditions, aerosol size distributions, aerosol mass concentrations, and single particle size and chemical composition in Bakersfield, CA for the period January 9, 1999 through January 28, 1999. The sampling period included four distinct meteorological periods of stagnation, clearing, haze, and rain. Particle number and mass concentrations were the highest during the stagnation episode when a heavy and extensive fog developed. Mass and number concentrations also approached these high levels during the haze period. Single particle size and composition data from an aerosol time-of-flight mass spectrometer (ATOFMS) are used to provide unique continuous information on the diversity in types of particles present, the effects of meteorology on particle size and composition, and the distribution of important chemical species within individual particles. Aerosol composition and mixing state are found to vary with meteorological conditions. Single particle data show that carbonaceous aerosol with secondary ammonium, nitrate, and sulfate dominate the aerosol concentration during a stagnation period with a dramatic composition shift occurring to sodium type particles during the haze period. The aerosol is internally mixed with respect to carbon, nitrate, sulfate, and ammonium during the stagnation period. The mixing state changes significantly over the haze period when much greater diversity in the associations of chemical species within individual particles occurs.


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