Environ. Sci. Technol., 36 (22), 4868 -4879, 2002. 10.1021/es015823i S0013-936X(01)05823-0
Web Release Date: October 19, 2002

Copyright © 2002 American Chemical Society

A Field-Based Approach for Determining ATOFMS Instrument Sensitivities to Ammonium and Nitrate

Prakash V. Bhave

Department of Environment Science and Engineering, California Institute of Technology, Pasadena, California 91125-7800

Jonathan O. Allen

Departments of Chemical & Materials Engineering and Civil & Environmental Engineering, Arizona State University, Tempe, Arizona 82876-6006

Bradley D. Morrical and David P. Fergenson

Department of Chemistry, University of California, Riverside, Riverside, California 92521

Glen R. Cass

School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 39332-0340

Kimberly A. Prather*

Department of Chemistry and Biochemistry, University of California, San Diego, La Jolla, California 92093-0314

Received for review December 3, 2001

Revised manuscript received July 25, 2002

Accepted August 21, 2002

Abstract:

Aerosol time-of-flight mass spectrometry (ATOFMS) instruments measure the size and chemical composition of individual particles in real-time. ATOFMS chemical composition measurements are difficult to quantify, largely because the instrument sensitivities to different chemical species in mixed ambient aerosols are unknown. In this paper, we develop a field-based approach for determining ATOFMS instrument sensitivities to ammonium and nitrate in size-segregated atmospheric aerosols, using tandem ATOFMS-impactor sampling. ATOFMS measurements are compared with collocated impactor measurements taken at Riverside, CA, in September 1996, August 1997, and October 1997. This is the first comparison of ion signal intensities from a single-particle instrument with quantitative measurements of atmospheric aerosol chemical composition. The comparison reveals that ATOFMS instrument sensitivities to both and decline with increasing particle aerodynamic diameter over a 0.32-1.8 m calibration range. The stability of this particle size dependence is tested over the broad range of fine particle concentrations (PM1.8 = 17.6 ± 2.0-127.8 ± 1.8 g m-3), ambient temperatures (23-35 C), and relative humidity conditions (21-69%), encountered during the field experiments. This paper describes a potentially generalizable methodology for increasing the temporal and size resolution of atmospheric aerosol chemical composition measurements, using tandem ATOFMS-impactor sampling.


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