As part of a pilot study into the chemical and physical properties of Austr
alian fine particles, a suite of aerosol samples was collected at Ti Tree B
end in Launceston, Tasmania, during June and July 1997. This period represe
nts midwinter in the Southern Hemisphere, a period when aerosol sources in
Launceston are dominated by smoke from domestic wood burning. This paper de
scribes the results from this measurement campaign, with the aim of assessi
ng the effect of wood smoke on the chemical and physical characteristics of
ambient aerosol. A micro orifice uniform deposit impactor (MOUDI) was used
to measure the size distributions of the aerosol from 0.05 to 20 mu m aero
dynamic diameter. Continuous measurements of fine particle mass were made u
sing a PM2.5 tapered element oscillating microbalance (TEOM) and light scat
tering coefficients at 530 nm were measured with nephelometers.
Mass size distributions tended to be bimodal, with the diameter of the domi
nant mode tending to smaller sizes with increases in total mass. Non-sea sa
lt potassium and polycyclic aromatic hydrocarbons (PAHs) were used as chemi
cal tracers for wood smoke. Wood smoke was found to increase absolute parti
cle mass (enough to regularly exceed air quality standards), and to concent
rate mass in a single mode below 1 mu m aerodynamic diameter. The acid-base
equilibrium of the aerosol was altered by the wood smoke source, with free
acidity hydrogen ion, non-sea salt sulfate, and ammonium concentrations be
ing higher and the concentration of all species, including nitrate (to diff
ering extents), focused in the fine particle size ranges. The wood smoke so
urce also heavily influenced the aerosol scattering efficiency, adding to a
strong diurnal cycle in both mass concentration and light scattering.