Size-resolved elemental composition of aerosol particles in greater Sydney in 2002–2003
Taleb Hallal A C , Gail P. Box A D , David D. Cohen B and Eduard Stelcer BA School of Physics, University of New South Wales, Sydney, NSW 2052, Australia.
B Australian Nuclear Science and Technology Organisation, Locked bag 2001, Kirrawee DC, NSW 2232, Australia.
C Present address: Boral Cement, Maldon Bridge Road, Maldon, NSW 2571, Australia.
D Corresponding author. Email: g.box@unsw.edu.au
Environmental Chemistry 10(4) 295-305 https://doi.org/10.1071/EN12194
Submitted: 10 December 2012 Accepted: 3 May 2013 Published: 2 August 2013
Environmental context. Atmospheric aerosols may either scatter or absorb solar radiation, potentially cooling or warming the planet. The warming–cooling effects of aerosols are determined by their optical properties, which depend on chemical composition. To better predict aerosol effects we need a good understanding of aerosol chemistry across a wide size range and geographic area. We report results of a study designed to increase understanding of the chemical composition of fine and coarse aerosols in Sydney.
Abstract. Between November 2002 and December 2003 samples of PM2.5 and PM10 (particulate matter less than 2.5- and 10-μm aerodynamic diameter) aerosols were collected at four sites in the Sydney Basin in order to determine the spatial and seasonal variation of size-resolved aerosol chemical composition in the Sydney region and relate this to aerosol optical properties. Accelerator-based ion beam analysis was used to determine the elemental composition and black carbon (BC) was determined using the laser integrating plate method. Aerosol species were determined by multiplying a marker element by a factor based on molecular weight ratios. Mass concentrations at the rural sites were lower than at the urban sites with an average PM2.5/PM10 mass ratio of 0.5–0.6 for all sites although at the urban sites it was 0.2–0.25 in summer. For all sites BC was the dominant element, followed by Na. For the urban sites this was followed by Cl suggesting sea salt and then the soil elements Al and Si. For the rural sites the soil elements Al, Si and Ca were more important than Cl, which was found to decrease away from the coast. Analysis of aerosol species shows that BC accounts for a larger portion of PM2.5 than PM10 and sea salt and sulfate levels are higher in summer than in winter.
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