Thermal volatilization properties of atmospheric nanoparticles

Thermal volatilization is explored as a means of inferring the chemical composition of atmospheric aerosol particles with diameters smaller than 10 nm (nanoparticles). Such particles contain too little mass for quantitative chemical determination by traditional analytical methods. Aerosols were subjected to increasing temperature in an oven and particle loss was measured as a function of temperature with the TSI model 3025 ultrafine condensation particle counter (UCPC), which is capable of counting particles with diameters as small as 3 nm. Particle nucleation was observed down stream of the oven when it was heated above about 400°C. To reduce this artifact, the sample air down stream of the oven was cooled to condense the hot gases and/or the freshly nucleated particles before they reached the UCPC. Controlled experiments were done with pure ammonium sulfate (NH₄)₂SO₄ particles. The experimental design was optimized based on the known concentration of pure (NH₄)₂SO₄ particles vaporized in the oven and the diffusion of this material to the walls of the sampling tube before the particle counter.