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Effective Density and Mixing State of Aerosol Particles in a Near-Traffic Urban Environment

Jenny RisslerErgonomics and Aerosol Technology, ‡Division of Nuclear Physics, and §Solid State Physics, Lund University , P.O. Box 118, SE-221 00, Lund, SwedenErik NordinAxel ErikssonNuclear physicsPatrik NilssonMia FroschNuclear physicsMoa K. SporreNuclear physicsAneta WierzbickaBirgitta SvenningssonNuclear physicsJakob LöndahlNuclear physicsMaria E. MessingStaffan SjögrenNuclear physicsJette Gjerke HemmingsenSection of Environmental Health, Dept. of Public Health, University of Copenhagen, Postboks 209, 1014 København K, DenmarkSteffen LoftSection of Environmental Health, Dept. of Public Health, University of Copenhagen, Postboks 209, 1014 København K, DenmarkJoakim PagelsErik SwietlickiNuclear physics
ABI

Аннотация

In urban environments, airborne particles are continuously emitted, followed by atmospheric aging. Also, particles emitted elsewhere, transported by winds, contribute to the urban aerosol. We studied the effective density (mass-mobility relationship) and mixing state with respect to the density of particles in central Copenhagen, in wintertime. The results are related to particle origin, morphology, and aging. Using a differential mobility analyzer-aerosol particle mass analyzer (DMA-APM), we determined that particles in the diameter range of 50-400 nm were of two groups: porous soot aggregates and more dense particles. Both groups were present at each size in varying proportions. Two types of temporal variability in the relative number fraction of the two groups were found: soot correlated with intense traffic in a diel pattern and dense particles increased during episodes with long-range transport from polluted continental areas. The effective density of each group was relatively stable over time, especially of the soot aggregates, which had effective densities similar to those observed in laboratory studies of fresh diesel exhaust emissions. When heated to 300 °C, the soot aggregate volatile mass fraction was ∼10%. For the dense particles, the volatile mass fraction varied from ∼80% to nearly 100%.

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