Emissions and ambient distributions of Biogenic Volatile Organic Compounds (BVOC) in a ponderosa pine ecosystem: Interpretation of PTR-MS mass spectra

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Abstract

Two proton-transfer-reaction mass spectrometry systems were deployed at the Bio-hydro-atmosphere interactions of Energy, Aerosols, Carbon, H 2O2, Organics and Nitrogen-Southern Rocky Mountain 2008 field campaign (BEACHON-SRM08; July to September, 2008) at the Manitou Forest Observatory in a ponderosa pine woodland near Woodland Park, Colorado USA. The two PTR-MS systems simultaneously measured BVOC emissions and ambient distributions of their oxidation products. Here, we present mass spectral analysis in a wide range of masses (m/z40+ to 210+) to assess our understanding of BVOC emissions and their photochemical processing inside of the forest canopy. The biogenic terpenoids, 2-methyl-3-butene-2-ol (MBO, 50.2%) and several monoterpenes (MT, 33.5%) were identified as the dominant BVOC emissions from a transmission corrected mass spectrum (PTR-MS), averaged over the daytime (11 a.m. to 3 p.m., local time) of three days. To assess contributions of oxidation products of local BVOC, we calculate an oxidation product spectrum with the OH-and ozone-initiated oxidation product distribution mass spectra of two major BVOC emissions at the ecosystem (MBO andβ-pinene) that were observed from laboratory oxidation experiments. The majority (∼76%) of the total signal in the transmission corrected PTR-MS spectra could be explained by identified compounds. The remainder are attributed to oxidation products of BVOC emitted from nearby ecosystems and transported to the site, and oxidation products of unidentified BVOC emitted from the ponderosa pine ecosystem.

Figures

  • Table 1. A summary of fragmentation patterns of BVOC, relevant to this study. Major product ions (relative abundance > 10%) are listed and minor product ions are listed in the brackets at a drift tube energy of ∼120 Td.
  • Fig. 1. (a) An averaged mass spectrum and (b) an averaged transmission-corrected mass spectrum from branch enclosure measurements (11 a.m. to 3 p.m. of 12 August to 14 August 2008).
  • Table 2. Observed compounds/compound classes, product ions and abundances (%) in the transmission-corrected mass spectrum (3rd column). The proton transfer reaction rate corrected abundances (PTR Corr. Abd., %) along with proton transfer rate constants (PTR constants in 10−9 cm3 s−1) are also summarized in 6th and 5th column.
  • Table 3. Daily variations of emission rates of four BVOC observed from branch enclosures, measured by PTR-MS. Leaf cuvette measurement results are also summarized for measurements made at the same ecosystem with different ponderosa pine trees. Emission capacity (E30) and β (Guenther et al., 1993) derived from this study and previous studies of ponderosa pine in different ecosystems are also presented.
  • Fig. 2. Averaged diurnal variations of BVOC and their oxidation products for three weeks in the summer of 2008 (18 August to 6 September)
  • Fig. 3. Representative ambient mass spectra of (a) the daytime (2 to 3 p.m. on 14 August 2008) and (b) the nighttime (1 to 2 a.m. on 18 August 2008) periods. Their transmission corrected mass spectra are presented in (c) and (d), respectively.
  • Fig. 4. The transmission-corrected PTR-MS spectrum of the OH initiated MBO oxidation experiment.
  • Table 4. Major peaks in the ambient transmission corrected spectra and their normalized counts (Fig. 3).

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Kim, S., Karl, T., Guenther, A., Tyndall, G., Orlando, J., Harley, P., … Apel, E. (2010). Emissions and ambient distributions of Biogenic Volatile Organic Compounds (BVOC) in a ponderosa pine ecosystem: Interpretation of PTR-MS mass spectra. Atmospheric Chemistry and Physics, 10(4), 1759–1771. https://doi.org/10.5194/acp-10-1759-2010

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