Atmos. Chem. Phys. Discuss., 9, 19939-19966, 2009
www.atmos-chem-phys-discuss.net/9/19939/2009/
doi:10.5194/acpd-9-19939-2009
© Author(s) 2009. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Chirality and origin of atmospheric humic-like substances
I. Salma1, T. Mészáros1, W. Maenhaut2, E. Vass1, and Zs. Majer1
1Eötvös University, Institute of Chemistry, Budapest, Hungary
2Ghent University, Institute for Nuclear Sciences, Ghent, Belgium

Abstract. Aerosol water extracts and atmospheric humic-like substances (HULIS) obtained from PM2.5-fraction aerosol samples collected in a rural/continental background environment and in an urban environment in spring and summer, and at a tropical site that was heavily impacted by biomass burning were studied. Mean organic matter-to-organic carbon mass conversion factor and standard deviation of 2.04±0.06 were derived for HULIS from biomass burning. Mean atmospheric concentrations of HULIS for the rural and urban environments, and for the biomass burning during daylight periods and nights were 1.65, 2.2, 43, and 60 μg m, respectively. This indicates that intense emission sources and/or formation mechanisms of HULIS operate in biomass burning. Mean contributions of C in HULIS (HULIS-C) to water-soluble organic carbon (WSOC) were 35, 48, 63, and 76%, respectively, for the sample set listed. The data suggest that HULIS-C is the major component of the WSOC in tropical biomass burning, and that HULIS most likely do not share common origin in the three environments studied. Differentiation among the possible formation processes was attempted by investigating the optical activity of HULIS through their (electronic and vibrational) circular dichroism properties. The urban HULIS did not show optical activity, which is in line with the concept of their major airborne formation from anthropogenic aromatics. The rural HULIS revealed weak optical activity, which may be associated with one of their important formation pathways by photo-oxidation and oligomerisation, i.e., with the formation from chiral biogenic precursors with one of the enantiomers slightly enriched. The biomass burning HULIS exhibited strong effect in the vibrational circular dichroism as a clear distinction from the other two types. This was related to the contribution of the thermal degradation products of lignins and cellulose. The biomass burning HULIS resemble Suwannee River Fulvic Acid standard more closely in some aspects than the urban and rural types of HULIS, which may be related to their common origin from plant material.

Citation: Salma, I., Mészáros, T., Maenhaut, W., Vass, E., and Majer, Zs.: Chirality and origin of atmospheric humic-like substances, Atmos. Chem. Phys. Discuss., 9, 19939-19966, doi:10.5194/acpd-9-19939-2009, 2009.
 
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