Atmospheric Chemistry and Physics (Mar 2009)

Methyl chavicol: characterization of its biogenic emission rate, abundance, and oxidation products in the atmosphere

  • N. C. Bouvier-Brown,
  • A. H. Goldstein,
  • D. R. Worton,
  • D. M. Matross,
  • J. B. Gilman,
  • W. C. Kuster,
  • D. Welsh-Bon,
  • C. Warneke,
  • J. A. de Gouw,
  • T. M. Cahill,
  • R. Holzinger

Journal volume & issue
Vol. 9, no. 6
pp. 2061 – 2074

Abstract

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We report measurements of ambient atmospheric mixing ratios for methyl chavicol and determine its biogenic emission rate. Methyl chavicol, a biogenic oxygenated aromatic compound, is abundant within and above Blodgett Forest, a ponderosa pine forest in the Sierra Nevada Mountains of California. Methyl chavicol was detected simultaneously by three in-situ instruments – a gas chromatograph with mass spectrometer detector (GC-MS), a proton transfer reaction mass spectrometer (PTR-MS), and a thermal desorption aerosol GC-MS (TAG) – and found to be abundant within and above Blodgett Forest. Methyl chavicol atmospheric mixing ratios are strongly correlated with 2-methyl-3-buten-2-ol (MBO), a light- and temperature-dependent biogenic emission from the ponderosa pine trees at Blodgett Forest. Scaling from this correlation, methyl chavicol emissions account for 4–68% of the carbon mass emitted as MBO in the daytime, depending on the season. From this relationship, we estimate a daytime basal emission rate of 0.72–10.2 μgCg<sup>&minus;1</sup> h<sup>&minus;1</sup>, depending on needle age and seasonality. We also present the first observations of its oxidation products (4-methoxybenzaldehyde and 4-methyoxy benzene acetaldehyde) in the ambient atmosphere. Methyl chavicol is a major essential oil component of many plant species. This work suggests that methyl chavicol plays a significant role in the atmospheric chemistry of Blodgett Forest, and potentially other sites, and should be included explicitly in both biogenic volatile organic carbon emission and atmospheric chemistry models.