Optical properties of the San Joaquin Valley aerosol collected during the 1995 integrated monitoring study

Abstract Optical, filter chemistry, and cascade impactor data collected during the winter intensive of the IMS95 Study in the San Joaquin Valley (SJV) of California were analyzed to determine the light-extinction efficiency of aerosol species. Regression of light scattering by particles (bsp) measured by a heated nephelometer without a size selective inlet against PM2.5 front filter mass gave a scattering efficiency of 3.67±0.05 m2/g with an R2 (fraction of variance explained) of 0.94. Division of the aerosol into two components and applying two different corrections to the filter data for nitrate and organic carbon on the backup filter gave scattering efficiencies of 3.7±0.3 or 4.1±0.2 m2/g for the salts composed of sulfate, nitrate, and ammonium and 2.9±0.2 or 3.1±0.2 m2/g for all other species with R2 of 0.985 and 0.986. The ambient bsp measured by an open nephelometer was a simple function of PM2.5 mass and relative humidity (RH), giving R2 of 0.90 and 0.88 for two different RH sensors. Variations in PM2.5 size distribution and composition did not have an important effect on ambient bsp. The RH data from each sensor were repeatable enough to show the existence of a simple dependence of aerosol water uptake on RH, but RH sensor calibration uncertainties prevented determining this dependence. Inversion of MOUDI cascade impactor data gave sulfate and nitrate mass median diameters (MMD) between 0.4 and 0.8 μm. Mie scattering calculations based on MOUDI data provided humidity-dependent extinction efficiencies for the principal aerosol chemical species. These efficiencies combined with particle filter data showed that ammonium nitrate was the dominant contributor to wintertime light extinction. Source apportionment showed that light extinction was dominated by emissions sources contributing to the formation of secondary species, especially nitrate. These wintertime data are not expected to apply to summertime in the SJV.

[1]  J. Seinfeld,et al.  Continued development of a general equilibrium model for inorganic multicomponent atmospheric aerosols , 1987 .

[2]  J. Seinfeld,et al.  Atmospheric Gas-Aerosol Equilibrium I. Thermodynamic Model , 1993 .

[3]  R. Charlson,et al.  Optical characteristics of atmospheric aerosols , 1981 .

[4]  Judith C. Chow,et al.  Sensitivity of estimated light extinction coefficients to model assumptions and measurement errors , 1995 .

[5]  I. Tang,et al.  The relative importance of atmospheric sulfates and nitrates in visibility reduction , 1981 .

[6]  A. P. Waggoner,et al.  Intercomparison of integrating nephelometer measurements , 1981 .

[7]  Naresh Kumar,et al.  Spatial and temporal variations in PM10 and PM2.5 source contributions and comparison to emissions during the 1995 integrated monitoring study , 1999 .

[8]  W. Malm,et al.  The relative importance of soluble aerosols to spatial and seasonal trends of impaired visibility in the United States , 1994 .

[9]  C. Sloane Optical properties of aerosols of mixed composition , 1984 .

[10]  P. Solomon,et al.  The 1995-Integrated Monitoring Study (IMS95) of the California Regional PM10/PM2.5 Air Quality Study (CRPAQS) : Study overview : 1995 Integrated monitoring study , 1999 .

[11]  Warren H. White,et al.  Size-resolved measurements of light scattering by ambient particles in the southwestern U.S.A. , 1994 .

[12]  Hwa-Chi Wang,et al.  Adaptation of the Twomey Algorithm to the Inversion of Cascade Impactor Data , 1990 .

[13]  Peter H. McMurry,et al.  Issues in aerosol measurement for optics assessments , 1996 .