Articles | Volume 9, issue 13
Atmos. Chem. Phys., 9, 4387–4406, 2009
https://doi.org/10.5194/acp-9-4387-2009

Special issue: European Integrated Project on Aerosol-Cloud-Climate and Air...

Atmos. Chem. Phys., 9, 4387–4406, 2009
https://doi.org/10.5194/acp-9-4387-2009

  07 Jul 2009

07 Jul 2009

Photochemical production of aerosols from real plant emissions

Th. F. Mentel1, J. Wildt2, A. Kiendler-Scharr1, E. Kleist2, R. Tillmann1, M. Dal Maso1, R. Fisseha1, Th. Hohaus1, H. Spahn1, R. Uerlings2, R. Wegener1, P. T. Griffiths3, E. Dinar4, Y. Rudich4, and A. Wahner1 Th. F. Mentel et al.
  • 1Inst. for Chemistry and Dynamics of the Geosphere, Inst. 2: Troposphere, Research Centre Jülich, 52425 Jülich, Germany
  • 2Inst. for Chemistry and Dynamics of the Geosphere, Inst. 3: Phytosphere, Research Centre Jülich, 52425 Jülich, Germany
  • 3Centre for Atmospheric Science, Dept. of Chemistry, Lensfield Road, Univ. of Cambridge, Cambridge, CB2 1EW, UK
  • 4Dept. of Environmental Sciences, Weizmann Institute, Rehovot 76100, Israel

Abstract. Emission of biogenic volatile organic compounds (VOC) which on oxidation form secondary organic aerosols (SOA) can couple the vegetation with the atmosphere and climate. Particle formation from tree emissions was investigated in a new setup: a plant chamber coupled to a reaction chamber for oxidizing the plant emissions and for forming SOA. Emissions from the boreal tree species birch, pine, and spruce were studied. In addition, α-pinene was used as reference compound. Under the employed experimental conditions, OH radicals were essential for inducing new particle formation, although O3 (≤80 ppb) was always present and a fraction of the monoterpenes and the sesquiterpenes reacted with ozone before OH was generated. Formation rates of 3 nm particles were linearly related to the VOC carbon mixing ratios, as were the maximum observed volume and the condensational growth rates. For all trees, the threshold of new particle formation was lower than for α-pinene. It was lowest for birch which emitted the largest fraction of oxygenated VOC (OVOC), suggesting that OVOC may play a role in the nucleation process. Incremental mass yields were ≈5% for pine, spruce and α-pinene, and ≈10% for birch. α-Pinene was a good model compound to describe the yield and the growth of SOA particles from coniferous emissions. The mass fractional yields agreed well with observations for boreal forests. Despite the somewhat enhanced VOC and OH concentrations our results may be up-scaled to eco-system level. Using the mass fractional yields observed for the tree emissions and weighting them with the abundance of the respective trees in boreal forests SOA mass concentration calculations agree within 6% with field observations. For a future VOC increase of 50% we predict a particle mass increase due to SOA of 19% assuming today's mass contribution of pre-existing aerosol and oxidant levels.

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