Abstract
Abstract. Benzene cluster cations were revisited as a sensitive and selective reagent ion for the chemical ionization of dimethyl sulfide (DMS) and a select group of volatile organic compounds (VOCs). Laboratory characterization was performed using both a new set of compounds (i.e., DMS, β-caryophyllene) as well as previously studied VOCs (i.e., isoprene, α-pinene). Using a field deployable chemical-ionization time-of-flight mass spectrometer (CI-ToFMS), benzene cluster cations demonstrated high sensitivity (> 1 ncps ppt−1) to DMS, isoprene, and α-pinene standards. Parallel measurements conducted using a chemical-ionization quadrupole mass spectrometer, with a much weaker electric field, demonstrated that ion–molecule reactions likely proceed through a combination of ligand-switching and direct charge transfer mechanisms. Laboratory tests suggest that benzene cluster cations may be suitable for the selective ionization of sesquiterpenes, where minimal fragmentation (< 25 %) was observed for the detection of β-caryophyllene, a bicyclic sesquiterpene. The in-field stability of benzene cluster cations using CI-ToFMS was examined in the marine boundary layer during the High Wind Gas Exchange Study (HiWinGS). The use of benzene cluster cation chemistry for the selective detection of DMS was validated against an atmospheric pressure ionization mass spectrometer, where measurements from the two instruments were highly correlated (R2 > 0.95, 10 s averages) over a wide range of sampling conditions.
Highlights
Volatile organic compounds (VOCs) play a central role in atmospheric chemistry by regulating tropospheric ozone and secondary organic aerosol (SOA) production rates (Goldstein and Galbally, 2007)
Recent studies have shown that sesquiterpenes (SQT; C15H24) may play a significant role in secondary organic aerosol production (Jaoui et al, 2013 and others), but far less is known about their global emission rates (Guenther et al, 2012; Kanakidou et al, 2005)
Field measurements from the remote North Atlantic boundary layer were validated against simultaneous measurements of dimethyl sulfide (DMS) made by an atmospheric pressure ionization mass spectrometer with an isotopically labeled standard (APIMS-ILS) (Blomquist et al, 2010)
Summary
Volatile organic compounds (VOCs) play a central role in atmospheric chemistry by regulating tropospheric ozone and secondary organic aerosol (SOA) production rates (Goldstein and Galbally, 2007). The most complete and recent work on benzene ion chemistry, with application to atmospheric measurements, is from two papers by Leibrock and Huey, where the potential for benzene cations in the detection of isoprene and monoterpenes, among a suite of other conjugated dienes and aromatics, was discussed. 8.6 eV) than the monomer (Grover et al, 1987) It follows that benzene ion chemistry should be a sensitive measurement for a host of molecules of interest to the study of marine air, including DMS (IE = 8.6 eV), monoterpenes (IE = 8.07 eV, α-pinene), sesquiterpenes (IE = 8.3 eV, β-caryophyllene), and their first-generation oxidation products, as well as a host of atmospheric amines (through R2) (Al-Joboury and Turner, 1964; Hunter and Lias, 1998; McDiarmid, 1974). Field measurements from the remote North Atlantic boundary layer were validated against simultaneous measurements of DMS made by an atmospheric pressure ionization mass spectrometer with an isotopically labeled standard (APIMS-ILS) (Blomquist et al, 2010)
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