Abstract

Abstract. Volatile organic compound (VOC) mixing ratios measured by five independent instruments are compared at a forested site dominated by ponderosa pine (Pinus Ponderosa) during the BEACHON-ROCS field study in summer 2010. The instruments included a Proton Transfer Reaction Time of Flight Mass Spectrometer (PTR-TOF-MS), a Proton Transfer Reaction Quadrupole Mass Spectrometer (PTR-MS), a Fast Online Gas-Chromatograph coupled to a Mass Spectrometer (GC/MS; TOGA), a Thermal Dissociation Chemical Ionization Mass Spectrometer (PAN-CIMS) and a Fiber Laser-Induced Fluorescence Instrument (FILIF). The species discussed in this comparison include the most important biogenic VOCs and a selected suite of oxygenated VOCs that are thought to dominate the VOC reactivity at this particular site as well as typical anthropogenic VOCs that showed low mixing ratios at this site. Good agreement was observed for methanol, the sum of the oxygenated hemiterpene 2-methyl-3-buten-2-ol (MBO) and the hemiterpene isoprene, acetaldehyde, the sum of acetone and propanal, benzene and the sum of methyl ethyl ketone (MEK) and butanal. Measurements of the above VOCs conducted by different instruments agree within 20%. The ability to differentiate the presence of toluene and cymene by PTR-TOF-MS is tested based on a comparison with GC-MS measurements, suggesting a study-average relative contribution of 74% for toluene and 26% for cymene. Similarly, 2-hydroxy-2-methylpropanal (HMPR) is found to interfere with the sum of methyl vinyl ketone and methacrolein (MVK + MAC) using PTR-(TOF)-MS at this site. A study-average relative contribution of 85% for MVK + MAC and 15% for HMPR was determined. The sum of monoterpenes measured by PTR-MS and PTR-TOF-MS was generally 20–25% higher than the sum of speciated monoterpenes measured by TOGA, which included α-pinene, β-pinene, camphene, carene, myrcene, limonene, cineole as well as other terpenes. However, this difference is consistent throughout the study, and likely points to an offset in calibration, rather than a difference in the ability to measure the sum of terpenes. The contribution of isoprene relative to MBO inferred from PTR-MS and PTR-TOF-MS was smaller than 12% while GC-MS data suggested an average of 21% of isoprene relative to MBO. This comparison demonstrates that the current capability of VOC measurements to account for OH reactivity associated with the measured VOCs is within 20%.

Highlights

  • Solid EarthThe oxidation of volatile organic compounds (VOCs) plays a central role in atmospheric chemistry by fueling ozonePublished by Copernicus Publications on behalf of the European Geosciences Union

  • During the BEACHON-Rocky Mountain Organic Carbon Study (ROCS) field campaign in summer of 2010 a suite of instruments for VOC, nitrogen species, and oxidant measurements were combined with different sampling systems to probe soil and branch emissions, as well as ecosystem scale flux emissions

  • The results suggest that the overall ratio calculated from Proton Transfer Reaction Quadrupole Mass Spectrometer (PTR-MS) and PTR-time of flight mass analyzer (TOF-MS) presented here should be accurate to within 25 %

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Summary

Introduction

The oxidation of volatile organic compounds (VOCs) plays a central role in atmospheric chemistry by fueling ozone. In addition to the real-time VOC measurements, whole air canisters were sampled at the site regularly throughout the study and analyzed post-study using a multi-column, multi-detector laboratory GC technique (Zhou et al, 2008; Russo et al, 2010). To our knowledge this is the first time that this set of different VOC techniques are compared under natural conditions above a ponderosa pine forest for several days. It will serve to improve our ability to measure VOCs in a forested environment

Experimental
Field site
PTR-TOF-MS and PTR-MS
PAN-CIMS
Findings
Conclusions
Full Text
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