Abstract

Eddy covariance (EC) is the preferable technique for flux measurements since it is the only direct flux determination method. It requires a continuum of high time resolution measurements (e.g. 5-20 Hz). For volatile organic compounds (VOC) soft ionization via proton transfer reaction has proven to be a quantitative method for real time mass spectrometry; here we use a proton transfer reaction time of flight mass spectrometer (PTR-TOF) for 10 Hz EC measurements of full mass spectra up to m/z 315. The mass resolution of the PTR-TOF enabled the identification of chemical formulas and separation of oxygenated and hydrocarbon species exhibiting the same nominal mass. We determined 481 ion mass peaks from ambient air concentration above a managed, temperate mountain grassland in Neustift, Stubai Valley, Austria. During harvesting we found significant fluxes of 18 compounds distributed over 43 ions, including protonated parent compounds, as well as their isotopes and fragments and VOC-H+ - water clusters. The dominant BVOC fluxes were methanol, acetaldehyde, ethanol, hexenal and other C6 leaf wound compounds, acetone, acetic acid, monoterpenes and sequiterpenes. The smallest reliable fluxes we determined were less than 0.1 nmol m-2 s-1, as in the case of sesquiterpene emissions from freshly cut grass. Terpenoids, including mono- and sesquiterpenes, were also deposited to the grassland before and after the harvesting. During cutting, total VOC emission fluxes up to 200 nmolC m-2 s-1 were measured. Methanol emissions accounted for half of the emissions of oxygenated VOCs and a third of the carbon of all measured VOC emissions during harvesting.

Highlights

  • Traditional flux measurement techniques of volatile organic compounds (VOCs) using proton-transfer-reaction – massspectrometry (PTR-MS) enable either eddy covariance (EC) measurement of one compound or disjunct eddy covariance (DEC) of several selected volatile organic compounds (e.g. Karl et al, 2001a)

  • The simultaneous flux of water can influence fluxes observed for VOCs with humidity influenced detection

  • PTR – time-of-flight (PTR-TOF) allowed scanning a wide range of VOCs

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Summary

Introduction

Traditional flux measurement techniques of volatile organic compounds (VOCs) using proton-transfer-reaction – massspectrometry (PTR-MS) enable either eddy covariance (EC) measurement of one compound or disjunct eddy covariance (DEC) of several selected volatile organic compounds (e.g. Karl et al, 2001a). Conventional PTR-MS uses a quadrupole mass filter which allows measuring one mass at a time with a mass separation capability of one atomic mass unit. The newly developed PTR – time-of-flight (PTR-TOF) (Graus et al, 2010; Jordan et al, 2010) can measure 10 Hz time series of full mass spectra with a mass accuracy sufficient to determine chemical formulas (i.e. separate oxygen containing VOCs from pure hydrocarbons). Data processing methods of continuous high-time and high-mass resolution PTR-TOF data has previously been described by Graus et al (2010). It was demonstrated that a mass resolution of 4400 m/ m and a mass accuracy of 2.5 ppm can be achieved if internal calibrations of the temperature dependent mass scale are continuously performed.

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