Atmos. Chem. Phys. Discuss., 10, 4753-4788, 2010
www.atmos-chem-phys-discuss.net/10/4753/2010/
doi:10.5194/acpd-10-4753-2010
© Author(s) 2010. 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.
The chemical and microphysical properties of secondary organic aerosols from Holm Oak emissions
N. Lang-Yona1, Y. Rudich1, Th. F. Mentel2, A. Buchholz2, A. Kiendler-Scharr2, E. Kleist2, C. Spindler2, R. Tillmann2, and J. Wildt2
1Department of Environmental Sciences, Weizmann Institute, Rehovot, 76100, Israel
2Institut für Chemie und Dynamik der Geosphäre (ICG), Forschungszentrum Jülich GmbH, Jülich, Germany

Abstract. The Mediterranean region is expected to experience substantial climatic change in the next 50 years. But, possible effects of climate change on biogenic volatile organic compound (VOC) emissions as well as on the formation of secondary organic aerosols (SOA) produced from these VOC are yet unexplored. To address such issues, the effects of temperature and light intensity on the VOC emissions of Mediterranean Holm Oak have been studied in the Jülich plant aerosol atmosphere chamber, as well as the optical and microphysical properties of the resulting SOA.

Monoterpenes dominated the VOC emissions from Holm Oak (97.5%) and temperature increase enhanced the emission strength under variation of the emission pattern. The amount of SOA increased linearly with the emission strength with a fractional mass yield of 5.7±1%, independent of the detailed emission pattern. The particles were highly scattering with no absorption abilities. Their average hygroscopic growth factor was 1.13±0.03 at 90% RH with a critical diameter of droplet activation of 100±4 nm at a supersaturation of 0.4%. All microphysical properties did not depend on the detailed emission pattern, in accordance with an invariant O/C ratio (0.57(+0.03/−0.1)) of the SOA observed by high resolution aerosol mass spectrometry.

The increase of Holm oak emissions with temperature (≈20% per degree) was stronger than e.g. for Boreal tree species (≈10% per degree). Increasing mean temperature in Mediterranean areas therefore may have a stronger impact on VOC emissions and SOA formation than in areas with Boreal forests.


Citation: Lang-Yona, N., Rudich, Y., Mentel, Th. F., Buchholz, A., Kiendler-Scharr, A., Kleist, E., Spindler, C., Tillmann, R., and Wildt, J.: The chemical and microphysical properties of secondary organic aerosols from Holm Oak emissions, Atmos. Chem. Phys. Discuss., 10, 4753-4788, doi:10.5194/acpd-10-4753-2010, 2010.
 
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