Abstract

Abstract. During summer 2010, a proton transfer reaction – time of flight – mass spectrometer (PTR-TOF-MS) and a quadrupole proton transfer reaction mass spectrometer (PTR-MS) were deployed simultaneously for one month in an orange orchard in the Central Valley of California to collect continuous data suitable for eddy covariance (EC) flux calculations. The high time resolution (5 Hz) and high mass resolution (up to 5000 m/Δm) data from the PTR-TOF-MS provided the basis for calculating the concentration and flux for a wide range of volatile organic compounds (VOC). Throughout the campaign, 664 mass peaks were detected in mass-to-charge ratios between 10 and 1278. Here we present PTR-TOF-MS EC fluxes of the 27 ion species for which the vertical gradient was simultaneously measured by PTR-MS. These EC flux data were validated through spectral analysis (i.e., co-spectrum, normalized co-spectrum, and ogive). Based on inter-comparison of the two PTR instruments, no significant instrumental biases were found in either mixing ratios or fluxes, and the data showed agreement within 5% on average for methanol and acetone. For the measured biogenic volatile organic compounds (BVOC), the EC fluxes from PTR-TOF-MS were in agreement with the qualitatively inferred flux directions from vertical gradient measurements by PTR-MS. For the 27 selected ion species reported here, the PTR-TOF-MS measured total (24 h) mean net flux of 299 μg C m−2 h−1. The dominant BVOC emissions from this site were monoterpenes (m/z 81.070 + m/z 137.131 + m/z 95.086, 34%, 102 μg C m−2 h−1) and methanol (m/z 33.032, 18%, 72 μg C m−2 h−1). The next largest fluxes were detected at the following masses (attribution in parenthesis): m/z 59.048 (mostly acetone, 12.2%, 36.5 μg C m−2 h−1), m/z 61.027 (mostly acetic acid, 11.9%, 35.7 μg C m−2 h−1), m/z 93.069 (para-cymene + toluene, 4.1%, 12.2 μg C m−2 h−1), m/z 45.033 (acetaldehyde, 3.8%, 11.5 μg C m−2 h−1), m/z 71.048 (methylvinylketone + methacrolein, 2.4%, 7.1 μg C m−2 h−1), and m/z 69.071 (isoprene + 2-methyl-3-butene-2-ol, 1.8%, 5.3 μg C m−2 h−1). Low levels of emission and/or deposition (<1.6% for each, 5.8% in total flux) were observed for the additional reported masses. Overall, our results show that EC flux measurements using PTR-TOF-MS is a powerful new tool for characterizing the biosphere-atmosphere exchange including both emission and deposition for a large range of BVOC and their oxidation products.

Highlights

  • Quantifying both emission and deposition of atmospheric volatile organic compounds (VOC) and their oxidation products is critical in understanding their roles in tropospheric chemistry, their contributions to photochemical production of ozone (O3) and secondary organic aerosol (SOA) (Chameides et al, 1988; Andreae and Crutzen, 1997; Fuentes et al, 2000; Jang et al, 2002; Goldstein and Galbally, 2007)

  • We focus on 27 ion species including all those selected for proton transfer reaction-mass spectrometer (PTR-MS) flux and vertical gradient measurement, acetic acid (m/z 61.027), and a major fragment of terpenes (m/z 95.086) which showed significant flux

  • We show the average diurnal flux of acetic acid detected by PTR-TOF-MS, because it was one of the species emitted in highest quantity, its vertical gradients were not measured by PTR-MS

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Summary

Introduction

Quantifying both emission and deposition of atmospheric volatile organic compounds (VOC) and their oxidation products is critical in understanding their roles in tropospheric chemistry, their contributions to photochemical production of ozone (O3) and secondary organic aerosol (SOA) (Chameides et al, 1988; Andreae and Crutzen, 1997; Fuentes et al, 2000; Jang et al, 2002; Goldstein and Galbally, 2007). Biogenic volatile organic compounds (BVOC) emissions from vegetation are estimated to be an order of magnitude larger than those from fossil fuel combustion, so BVOC emissions constitute approximately 90 % of global VOC emissions (Guenther et al, 1995). In present BVOC emission models such as the Biogenic Emission Inventory System (BEIS, Pierce et al, 1998) and the Model of Emissions of Gases and Aerosols from Nature (MEGAN, Guenther et al, 2006), there are additional uncertainties for example in estimating the VOC fluxes by up-scaling from leaf-level measurements to the ecosystem or landscape scale. Bouvier-Brown et al (2009) and Ciccioli et al (1999) detected much less emission of sesquiterpenes above plant canopies compared to the amount measured from branch enclosure tests, revealing significant losses of the sesquiterpenes before they escape the plant canopy due to their high reactivity

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