Yc. Chan et al., Characterisation and source identification of PM10 aerosol samples collected with a high volume cascade impactor in Brisbane (Australia), SCI TOTAL E, 262(1-2), 2000, pp. 5-19
PM10 (particulate matter with aerodynamic diameter < 10 mu m) samples of Br
isbane air were collected and fractionated into six size fractions (< 0.5,
0.5-0.61, 0.61-1.3, 1.3-2.7, 2.7-4.9 and 4.9-10 mu m) with a high volume ca
scade impactor. The chemical composition of the samples was analysed by tec
hniques including Ion Beam Analysis. On average, 42% of the aerosol mass is
in the > 2.7-mu m size fraction, with the <0.5-mu m size fraction also con
tributes 41% of the aerosol mass. The composition of the < 1.3-mu m aerosol
s is significantly different to that of the > 1.3-mu m aerosols. The aeroso
l mass and concentrations of chemical components related to human activitie
s show a bimodal size-distribution pattern, with most of the mass in the ac
cumulation range (< 0.65 mu m). The size geometric mean of aerosol mass is
0.96 mu m in the samples collected from an industrial/residential site, and
is 1.74 mu m in the samples collected from a suburban site. The size geome
tric mean of concentrations of chemical components related to human activit
ies ranges from 0.16 to 0.57 mu m. The concentrations of crustal matter and
sea salt show a unimodal size-distribution pattern, and with geometric mea
ns of 3.73 and 4.12 mu m, respectively. Four source factors were resolved b
y multivariate analysis techniques for the size-fractionated aerosol sample
s, namely the soil, sea salt, organics and vehicular exhausts factors. The
source fingerprints of the factors vary in the size ranges and have implica
tions on the formation and dispersal processes of the particles. On average
, the soil and sea salt factors contribute more than 80% of the aerosol mas
s in the > 2.7-mu m fractions, while the organics and vehicular exhausts fa
ctors explain almost all the aerosol mass in the < 0.61-mu m fractions. (C)
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