Field validation of a semi-continuous method for aerosol black carbon (aethalometer) and temporal patterns of summertime hourly black carbon measurements in southwestern PA
Ga. Allen et al., Field validation of a semi-continuous method for aerosol black carbon (aethalometer) and temporal patterns of summertime hourly black carbon measurements in southwestern PA, ATMOS ENVIR, 33(5), 1999, pp. 817-823
Two methods for measuring aerosol elemental carbon (EC) are compared. Three
-hour integrated carbon samples were collected on quartz filters during the
summer of 1990 in Uniontown, PA, primarily during episodes of elevated par
ticulate pollution levels. These samples were analyzed for EC and organic c
arbon (OC) using a thermo/optical reflectance (TOR) method. Aerosol black c
arbon (BC) was measured using an Aethalometer, a semi-continuous optical ab
sorption method. The optical attenuation factor for ambient BC was supplied
by the instrument manufacturer. Three-hour average concentrations were cal
culated from the semi-continuous BC measurements to temporally match the EC
/OC integrated quartz filter samples. BC and EC concentrations are highly c
orrelated over the study period (R-2 = 0.925). The regression equation is B
C (mu g m(-3)) = 0.95 (+/- 0.04) EC - 0.2 (+/- 0.4). The means of 3 h avera
ge measurements for EC and BC are 2.3 and 2.0 mu g m(-3), respectively, ave
rage concentrations of EC and BC ranged from 0.6 to 9.4 and 0.5 to 9.0 mu g
m(-3) respectively. TOR OC and EC concentrations were not highly correlate
d (R-2 = 0.22). The mean OC/EC ratio was 1.85.
The 10-week Aethalometer hourly dataset was analyzed for daily and weekly t
emporal patterns. A strong diurnal BC pattern was observed, with peaks occu
rring between 7 a.m. and 9 a.m. local time. This is consistent with the inc
rease in emissions from ground level combustion sources in the morning, cou
pled with poor dispersion before daytime vertical mixing is established. Th
ere was also some indication of a day-of-week effect on BC concentrations,
attributed to activity of local ground level anthropogenic sources. Compari
son of BC concentrations with co-located measurements of coefficient of haz
e in a separate field study in Philadelphia, PA, during the summer of 1992
showed good correlation between the two measurements (R-2 = 0.82). (C) 1999
Published by Elsevier Science Ltd. All rights reserved.