Light degrading properties of size-fractionated PM10 aerosol samples collected from an industrial area in Brisbane, Australia

被引:3
作者
Chan, YC [1 ]
McTainsh, GH
Simpson, RW
Vowles, PD
Cohen, DD
Bailey, GM
机构
[1] Griffith Univ, Australian Sch Environm Studies, Nathan, Qld 4111, Australia
[2] Univ Sunshine Coast, Fac Sci, Sippy Downs, Vic, Australia
[3] Australian Nucl Sci & Technol Org, Menai, NSW 2234, Australia
关键词
D O I
10.1080/02786820290038537
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
Thirty-seven days of PM10 aerosol samples (particles with aerodynamic diameter <10 μm) were collected in an industrial area in Brisbane during April to June 1999 to study the light extinction efficiencies of urban aerosols in different size ranges. The light scattering coefficient of the air was measured by nephelometry. The light absorption coefficient of the aerosol samples was measured by the integrating plate laser absorption method. Multiple linear regression techniques were used to investigate the relationships between the visibility degrading properties and the chemical composition of the aerosol samples. The results are comparable with those from other visual air quality studies. The absorption of light by fine (PM2.5) aerosols is mainly due to elemental carbon (EC) particles smaller than 0.5 μm. The b(ap)(0) values of EC particles in different size ranges are 9.08 (<2.7 μm) and 0.32 (2.7-10 μm)m(2)g(1), respectively. The absorption of light by coarse (PM2.5-10) aerosols is mainly due to soil (b(ap)(0) = 0.17) and organic (b(ap)(0) = 1.11) particles. The scattering of light is highly related to the concentration of fine particles in the air (mass scattering efficiency b(sp)(0) = 1.65) and is mainly due to the fine sulphate (b(sp)(0) = 10.9), soil (b(sp)(0) = 2.73), and EC (b(sp)(0) = 3.89) particles. On average, fine EC (44%), sulphate (20%) and soil (7%) particles, NO2 (9%), and Rayleigh scattering (19%) were the largest contributors of visibility degradation for the sampling days in this study.
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页码:890 / 898
页数:9
相关论文
共 46 条
[1]  
ANDERSON KR, 1992, J AIR WASTE MANAGEME, V42, P771
[2]   VISIBILITY AS RELATED TO ATMOSPHERIC AEROSOL CONSTITUENTS [J].
APPEL, BR ;
TOKIWA, Y ;
HSU, J ;
KOTHNY, EL ;
HAHN, E .
ATMOSPHERIC ENVIRONMENT, 1985, 19 (09) :1525-1534
[3]  
AYERS GP, 1990, CLEAN AIR, V24, P18
[4]  
Bentley ST, 1991, CSIRO EPA MELBOURNE
[5]  
Bohren C. F., 1998, ABSORPTION SCATTERIN
[6]   Calibration and intercomparison of filter-based measurements of visible light absorption by aerosols [J].
Bond, TC ;
Anderson, TL ;
Campbell, D .
AEROSOL SCIENCE AND TECHNOLOGY, 1999, 30 (06) :582-600
[7]   Light absorption by primary particle emissions from a lignite burning plant [J].
Bond, TC ;
Bussemer, M ;
Wehner, B ;
Keller, S ;
Charlson, RJ ;
Heintzenberg, J .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1999, 33 (21) :3887-3891
[8]   INDIRECT MEASUREMENT OF HYDROCARBON AEROSOLS ACROSS THE UNITED-STATES BY NONSULFATE HYDROGEN-REMAINING GRAVIMETRIC MASS CORRELATIONS [J].
CAHILL, TA ;
ELDRED, RA ;
MOTALLEBI, N ;
MALM, WC .
AEROSOL SCIENCE AND TECHNOLOGY, 1989, 10 (02) :421-429
[9]   Aerosol light scattering properties at Cape Grim, Tasmania, during the First Aerosol Characterization Experiment (ACE 1) [J].
Carrico, CM ;
Rood, MJ ;
Ogren, JA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D13) :16565-16574
[10]   RELATIONSHIP BETWEEN SULFATE AIR-QUALITY AND VISIBILITY WITH EXAMPLES IN LOS-ANGELES [J].
CASS, GR .
ATMOSPHERIC ENVIRONMENT, 1979, 13 (08) :1069-1084