EGU24-16012, updated on 09 Mar 2024
https://doi.org/10.5194/egusphere-egu24-16012
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Apportionment of absorption in complex aerosols in South Africa

Clarissa Baldo1, Brigitte Language2, Tommaso Isolabella3, Virginia Vernocchi4, Dario Massabò3, Claudia Di Biagio5, Pieter Van Zyl6, Stuart Piketh6, and Paola Formenti5
Clarissa Baldo et al.
  • 1Université Paris Cité and Univ Paris Est Creteil, CNRS, LISA, F-75013 Paris, France; now at Univ Paris Est Creteil and Université Paris Cité, CNRS, LISA, F-94010 Créteil, France
  • 2Univ Paris Est Creteil and Université Paris Cité, CNRS, LISA, F-94010 Créteil, France; now at Unit for Environmental Sciences and Management, North-West University, Potchefstroom 2520, South Africa
  • 3Physics Department, University of Genoa, 16146 Genoa, Italy
  • 4I.N.F.N., Division of Genoa, 16146 Genoa, Italy
  • 5Université Paris Cité and Univ Paris Est Creteil, CNRS, LISA, F-75013 Paris, France
  • 6Unit for Environmental Sciences and Management, North-West University, Potchefstroom 2520, South Africa

South Africa, with its industrialised economy, faces unique air pollution challenges. Our study investigates aerosol composition and absorption in the Highveld region. Understanding aerosol absorption is critical as it affects climate, air quality, and public health. Aerosol absorption in the lower atmosphere affects the evolution of the boundary layer and the dispersion of pollutants, which in turn affects air quality and public health. Aerosol filter samples (PM10 fractions) were collected from residential, traffic, and industrial sites during the dry season. Chemical analyses, including X-ray fluorescence, thermo-optical analysis, and ion chromatography, were carried out to determine elemental species, carbonaceous species, and water-soluble ions, respectively. Based on this, a mass closure calculation was performed to define the contribution of five major aerosol components. The calculated aerosol mass concentrations were in good agreement with the measurements (Normalised Mean Bias, NMB < 7%). No significant variation in PM10 concentration was observed between site types. Mineral dust appeared to be the main contributor to PM10, varying from about 48%-60% at different sites, followed by organic matter (OM, 22%-35%), secondary inorganic aerosols (SIA, 9%-12%), elemental carbon (EC, 4%-7%), and sea salt (ss, 1%-2%).

Aerosol spectral absorption was obtained from multi-wavelength absorbance analysis (MWAA) measurements at 375, 407, 532, 635, and 850 nm. High absorption was measured in the following order: industrial> residential> traffic sites. The estimated absorption Ångström exponent (AAE) varied from 0.8 to 2 at different sites, indicating the contribution of several sources. At 850 nm absorption correlates well with EC as expected (r = 0.85). The obtained mass absorption efficiency (8 m2/g) is in line with expectations. Specific tracers were used to determine the contribution of the main absorbing aerosol components - black carbon (BC), brown organic carbon (BrC) from incomplete biomass combustion, and mineral dust - using correlations between estimated mass and measured absorption. Preliminary results indicate that although BC is the major contributor to absorption, accounting for 30%-60% absorption at 375 nm, followed by BrC 10%-50%, the contribution of the less absorbing but more abundant mineral dust is not negligible and can range from 2% to 50% in different samples. These results underline the complexity of aerosols in the region and their high absorption properties, and the need for a comprehensive understanding of its various components to accurately assess its impact.

How to cite: Baldo, C., Language, B., Isolabella, T., Vernocchi, V., Massabò, D., Di Biagio, C., Van Zyl, P., Piketh, S., and Formenti, P.: Apportionment of absorption in complex aerosols in South Africa, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-16012, https://doi.org/10.5194/egusphere-egu24-16012, 2024.