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

被引:40
作者
Richards, LW [1 ]
Alcorn, SH
McDade, C
Couture, T
Lowenthal, D
Chow, JC
Watson, JG
机构
[1] Sonoma Technol Inc, Petaluma, CA USA
[2] ENSR Corp, Camarillo, CA USA
[3] Univ Nevada, Desert Res Inst, Reno, NV 89506 USA
关键词
aerosol light-scattering efficiency; relative humidity; effect on light scattering; light-extinction budget; source apportionment of light extinction;
D O I
10.1016/S1352-2310(99)00267-8
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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 (b(sp)) 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 m(2)/g with an R-2 (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 3.1 +/- 0.2 m(2)/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 R-2 of 0.985 and 0.986. The ambient b(sp) measured by an open nephelometer was a simple function of PM2.5 mass and relative humidity (RH), giving R-2 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 b(sp). 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 mu m. 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. (C) 1999 Published by Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:4787 / 4795
页数:9
相关论文
共 25 条
[1]  
CHOW JC, 1997, 54601F1 DRI
[2]   ATMOSPHERIC GAS AEROSOL EQUILIBRIUM .1. THERMODYNAMIC MODEL [J].
KIM, YP ;
SEINFELD, JH ;
SAXENA, P .
AEROSOL SCIENCE AND TECHNOLOGY, 1993, 19 (02) :157-181
[3]   SENSITIVITY OF ESTIMATED LIGHT EXTINCTION COEFFICIENTS TO MODEL ASSUMPTIONS AND MEASUREMENT ERRORS [J].
LOWENTHAL, DH ;
RODGERS, CF ;
SAXENA, P ;
WATSON, JG ;
CHOW, JC .
ATMOSPHERIC ENVIRONMENT, 1995, 29 (07) :751-766
[4]  
MAGLIANO KL, 1998, ATMOSPHERIC ENV
[5]  
MCDADE CE, 1997, IMS95 DATA ANAL WORK
[6]   Issues in aerosol measurement for optics assessments [J].
McMurry, PH ;
Zhang, XQ ;
Lee, CT .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D14) :19189-19197
[7]  
MCMURRY PH, 1997, COMMUNICATION
[8]  
MOLENAR JV, 1998, UNPUB J AIR WASTE MA
[9]  
MOLENAR JV, 1992, 85 ANN M EXH AIR WAS
[10]   CONTINUED DEVELOPMENT OF A GENERAL EQUILIBRIUM-MODEL FOR INORGANIC MULTICOMPONENT ATMOSPHERIC AEROSOLS [J].
PILINIS, C ;
SEINFELD, JH .
ATMOSPHERIC ENVIRONMENT, 1987, 21 (11) :2453-2466