Atmos. Chem. Phys. Discuss., 11, 26111-26141, 2011
www.atmos-chem-phys-discuss.net/11/26111/2011/
doi:10.5194/acpd-11-26111-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Sources and composition of urban aerosol particles
M. Vogt1, C. Johansson1,2, M. Mårtensson1,3, H. Struthers1,4,5, L. Ahlm1, and D. Nilsson1
1Department of Applied Environmental Science (ITM), Stockholm University, 106 91 Stockholm, Sweden
2City of Stockholm Environment and Health Administration, Box 8136, 10420 Stockholm, Sweden
3Department of Earth Sciences, Uppsala University, 752 36 Uppsala, Sweden
4Department of Meteorology, Stockholm University, 10691 Stockholm, Sweden
5Bert Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden

Abstract. From May 2008 to March 2009 aerosol emissions were measured using the eddy covariance method covering the size range 0.25 to 2.5 μm diameter (Dp) from a 105 m tower, in central Stockholm, Sweden. Supporting chemical aerosol data were collected at roof and street level. Results show that the inorganic fraction of sulfate, nitrate, ammonium and sea salt accounts for approximately 15% of the total aerosol mass <1 μm Dp (PM1) with water soluble soil contributing 11% and water insoluble soil 47%. Carbonaceous compounds were at the most 27% of PM1 mass. It was found that heating the air from the tower to 200 °C resulted in the loss of approximately 60% of the aerosol volume at 0.25 μm Dp whereas only 40% of the aerosol volume was removed at 0.6 μm Dp. Further heating to 300 °C caused very little additional losses <0.6 μm Dp. The chemical analysis did not include carbonaceous compounds, but based on the difference between the total mass concentration and the sum of the analyzed non-carbonaceous materials, it can be assumed that the non-volatile particulate material (heated to 300 °C) consists mainly of carbonaceous compounds, including elemental carbon. Furthermore, it was found that the non-volatile particle fraction <0.6 μm Dp correlated (r2 = 0.4) with the BC concentration at roof level in the city, supporting the assumption that the non-volatile material consists of carbonaceous compounds. The average diurnal cycles of the BC emissions from road traffic (as inferred from the ratio of the incremental concentrations of nitrogen oxides (NOx) and BC measured on a densely trafficked street) and the fluxes of non-volatile material at tower level are in close agreement, suggesting a traffic source of BC. We have estimated the emission factors (EFs) for non-volatile particles <0.6 μm Dp to be 2.4±1.4 mg veh−1 km−1 based on either CO2 fluxes or traffic activity data. Light (LDV) and heavy duty vehicle (HDV) EFs were estimated using multiple linear regression and reveal that for non-volatile particulate matter in the 0.25 to 0.6 μm Dp range, the EFHDV is approximately twice as high as the EFLDV, the difference not being statistically significant.

Citation: Vogt, M., Johansson, C., Mårtensson, M., Struthers, H., Ahlm, L., and Nilsson, D.: Sources and composition of urban aerosol particles, Atmos. Chem. Phys. Discuss., 11, 26111-26141, doi:10.5194/acpd-11-26111-2011, 2011.
 
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