Abstract

Oxygenated volatile organic compounds (OVOC) can dominate atmospheric organic chemistry, but they are difficult to measure reliably at low levels in complex mixtures. Several techniques that have been used to speciate nonmethane organic compounds (NMOC) including OVOC were codeployed/intercompared in well‐mixed smoke generated by 47 fires in the U.S. Department of Agriculture Forest Service Fire Sciences Combustion Facility. The agreement between proton transfer reaction mass spectrometry (PTR‐MS) and open‐path Fourier transform infrared spectroscopy (OP‐FTIR) was excellent for methanol (PT/FT = 1.04 ± 0.118) and good on average for phenol (0.843 ± 0.845) and acetol (∼0.81). The sum of OP‐FTIR mixing ratios for acetic acid and glycolaldehyde agreed (within experimental uncertainty) with the PTR‐MS mixing ratios for protonated mass 61 (PT/FT = 1.17 ± 0.34), and the sum of OP‐FTIR mixing ratios for furan and isoprene agreed with the PTR‐MS mixing ratios for protonated mass 69 (PT/FT = 0.783 ± 0.465). The sum of OP‐FTIR mixing ratios for acetone and methylvinylether accounted for most of the PTR‐MS protonated mass 59 signal (PT/FT = 1.29 ± 0.81), suggesting that one of these compounds was underestimated by OP‐FTIR or that it failed to detect other compounds that could contribute at mass 59. Canister grab sampling followed by gas chromatography (GC) with mass spectrometry (MS), flame ionization detection (FID), and electron capture detection (ECD) analysis by two different groups agreed well with OP‐FTIR for ethylene, acetylene, and propylene. However, these propylene levels were below those observed by PTR‐MS (PT/FT = 2.33 ± 0.89). Good average agreement between PTR‐MS and GC was obtained for benzene and toluene. At mixing ratios above a few parts per billion the OP‐FTIR had advantages for measuring sticky compounds (e.g., ammonia and formic acid) or compounds with low proton affinity (e.g., hydrogen cyanide and formaldehyde). Even at these levels, only the PTR‐MS measured acetonitrile and acetaldehyde. Below a few ppbv only the PTR‐MS measured a variety of OVOC, but the possibility of fragmentation, interference, and sampling losses must be considered.

Highlights

  • Composition and Structure: Biosphere/atmosphere interactions; 0322 Atmospheric Composition and Structure: Constituent sources and sinks; 0365 Atmospheric Composition and Structure: Troposphere—composition and chemistry; 0394 Atmospheric Composition and Structure: Instruments and techniques; KEYWORDS: instrument intercomparision, biomass burning, oxygenated organic compounds

  • [30] As stated earlier, we found excellent agreement between Fourier transform infrared spectrometry (FTIR) and proton transfer reaction mass spectrometry (PTR-mass spectrometry (MS)) for methanol for all but one fire in this study and good overall agreement between cans and open-path Fourier transform infrared spectroscopy (OP-FTIR)

  • This suggests that larger differences that occurred for some other compounds were not due to incomplete mixing, sampling artifacts for ‘‘nonsticky’’ molecules, or instrument drift

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Summary

Introduction

[2] It is widely accepted that detailed models are needed to quantify the complex chemistry of the atmosphere. In the 1990s, it became clear that OVOC account for most of the NMOC from biomass burning [Griffith et al, 1991; Yokelson et al, 1996, 1997, 1999, 2003a; Worden et al, 1997; Holzinger et al, 1999] and a large fraction of the biogenic emissions from plants [Konig et al, 1995; Kirstine et al, 1998; Schade and Goldstein, 2001] Together these sources are estimated to produce more total trace gases and more VOC than the main global trace gas source: fossil fuel burning [Schimel et al, 1995; Andreae and Merlet, 2001; Guenther et al, 1995]. The canister techniques have been widely used for many years and provide analysis (with preconcentration) at ppt levels [Montzka et al, 1993] They may be subject to sampling and storage artifacts for trace gases that are unstable or sticky, which can comprise the majority of NMOC gases of interest in atmospheric chemistry studies. A detailed discussion of the emissions from African and Indonesian fuels used in this study appears in a companion paper [Christian et al, 2003]

Experiment
Trace Gas and Particle Instrumentation
Results and Discussion
Conclusions
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