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We present the application of time-of-flight mass spectrometry (TOF MS) for the analysis of halocarbons in the atmosphere after cryogenic sample preconcentration and gas chromatographic separation. For the described field of application, the quadrupole mass spectrometer (QP MS) is a state-of-the-art detector. This work aims at comparing two commercially available instruments, a QP MS and a TOF MS, with respect to mass resolution, mass accuracy, stability of the mass axis and instrument sensitivity, detector sensitivity, measurement precision and detector linearity. Both mass spectrometers are operated on the same gas chromatographic system by splitting the column effluent to both detectors. The QP MS had to be operated in optimised single ion monitoring (SIM) mode to achieve a sensitivity which could compete with the TOF MS. The TOF MS provided full mass range information in any acquired mass spectrum without losing sensitivity. Whilst the QP MS showed the performance already achieved in earlier tests, the sensitivity of the TOF MS was on average higher than that of the QP MS in the "operational" SIM mode by a factor of up to 3, reaching detection limits of less than 0.2 pg. Measurement precision determined for the whole analytical system was up to 0.2% depending on substance and sampled volume. The TOF MS instrument used for this study displayed significant non-linearities of up to 10% for two-thirds of all analysed substances.
In der vorliegenden Arbeit wurde ein Flugzeitmassenspektrometer (TOF-MS) für die Messung von halogenierten Spurengasen charakterisiert und das verwendete analytische System optimiert. Ein TOF-MS hat den Vorteil, dass es die volle Masseninformation aufzeichnet. Dadurch ist es möglich, auch im Nachhinein Substanzen zu identifizieren und retrospektiv auszuwerten. Eine retrospektive Auswertung kann helfen, Auswirkungen auf die Atmosphäre besser abschätzen zu können. Aus diesem Grund wurde mit Hilfe des TOF-MS ein digitales Datenarchiv durch regelmäßige Messungen von Luftproben, die am Taunus Observatorium auf dem Kleinen Feldberg genommen wurden, initialisiert. Durch die Wahl des Taunus Observatoriums werden in unmittelbarer Nähe des industriellen Ballungsraums Rhein-Main auf der Nordhemisphäre Luftproben genommen, wodurch die Wahrscheinlichkeit erhöht wird, unbekannte Substanzen in erhöhter Konzentration zu messen.
Bevor das TOF-MS jedoch für die Initialisierung des Datenarchivs verwendet werden konnte, wurde es charakterisiert und mit einem, für die Analyse von halogenierten Kohlenwasserstoffen etablierten QP-MS verglichen. Um beide Detektoren vergleichen zu können, erfolgte die Probenaufgabe, Probenaufkonzentrierung und die Separation der Probe im Gaschromatographen innerhalb eines gemeinsamen Systems. Nach der Separation im GC teilt sich der Trägergasfluss auf. Die Charakterisierung des TOF-MS und der Vergleich mit dem QP-MS umfasst die Auswertung der Daten, die Messpräzision, die Linearität, die Sensitivität der Detektoren, die Massenauflösung und die Massenachsenbestimmungsgenauigkeit.
Hinsichtlich der Messpräzision liegen beide Massenspektrometer, wie ermittelt auf dem selben Niveau, wodurch sie auch sehr geringe Variabilitäten in den Mischungsverhältnissen von halogenierten Kohlenwasserstoffen aufzeichnen können.
Die Linearität der Detektoren ist substanzspezifisch. Während das QP-MS in Übereinstimmung mit bereits literaturbekannter Eigenschaft, einen sehr großen linearen Bereich aufweist, zeigt das hier verwendete TOF-MS für 2/3 aller ausgewerteter Substanzen starke substanz- und fragmentabhängig Nichtlinearitäten. Das nichtlineare Verhalten des Detektors des TOF-MS zeigt sich auch bei den Messvergleichen, wobei jedoch nur signifikante Abweichungen bei sehr hohen und sehr niedrig gemessenen Mischungsverhältnissen beobachtet wurden. Diese starke Nichtlinearität stellt eine große Einschränkung für eine retrospektive Auswertung unbekannter Substanzen dar, da deren Verlauf nur qualitativ nicht aber quantitativ dargestellt werden kann.
Die Massenauflösung liegt beim TOF-MS bei 1000 mit einer Massenachsenbestimmungsgenauigkeit zwischen 50-170~ppm, wodurch es dem QP-MS, welches nur Einheitsauflösung vorweist, weit überlegen ist. Mit dieser Auflösung und Massenachsenbestimmungsgenauigkeit ist das TOF-MS in der Lage einen halogenierten von einem nichthalogenierten Kohlenwasserstoff quantitativ zu trennen.
Zum Vergleich der Sensitivität der beiden Massenspektrometer wurde das QP-MS in drei verschiedenen Modi betrieben: Zum einen dem SCAN-Modus, dem operationalen SIM-Modus, welcher im regulärem Messbetrieb verwendet wird und mehrere Ionen pro Zeitfenster misst, und dem optimierten SIM-Modus, welcher nur ein Ion der jeweiligen Substanz misst. Das TOF-MS hat die gleiche Sensitivität wie das QP-MS im optimierten SIM-Modus. Das TOF-MS hat eine um den Faktor 3 höhere Sensitivität als das QP-MS im operationalen SIM-Modus und eine um den Faktor 12 höhere Sensitivität als das QP-MS im SCAN-Modus bei den betrachteten Substanzen.
Die Initialisierung des digitalen Datenarchivs wurde im Oktober 2013 mit der Probennahme am Taunus Observatorium begonnen, wobei in der vorliegenden Arbeit der Zeitraum von einem Jahr betrachtet wurde. Es wurden Identifizierungen aus regulären Proben der Taunus Observatoriums-Zeitreihe durchgeführt und so die Substanzen HFC-32, HFC-245fa,HCFC-133a und HFO-1234yf gefunden. Zusätzlich stellte Martin Vollmer (Eidgenössische Material und Prüfgesellschaft) zwei Gasmischungen zu Verfügung für die Identifikation von noch nicht am System vermessenen Substanzen. Somit konnte die Vielfalt an diesem System vermessener Substanzen von 40 auf insgesamt 64 Substanzen erweitert werden.
Von den neu identifizierten Substanzen wurden HFC-227ea, HFC-236fa, HFC-32, HCFO-1233zd, HFO-1234zd, HFO-1234yf, HFC-245fa, HCFC-31, HFC-133a, Isofluran und HFC-112 in der Taunus Observatoriums-Zeitreihe gefunden und rückwirkend aufgearbeitet.
Durch die retrospektive Auswertung ist das TOF-MS für seine charakterisierte Anwendung zum Einsatz gekommen.
A new method for size resolved chemical analysis of nucleation mode aerosol particles (size range from ~10 to ~30 nm) is presented. The Thermal Desorption Differential Mobility Analyzer (TD-DMA) uses an online, discontinuous principle. The particles are charged, a specific size is selected by differential mobility analysis and they are collected on a filament by electrostatic precipitation. Subsequently, the sampled mass is evaporated in a clean carrier gas and analyzed by a chemical ionization mass spectrometer. Gas phase measurements are performed with the same mass spectrometer during the sampling of particles. The characterization shows reproducible results, with a particle size resolution of 1.19 and the transmission efficiency for 15 nm particles being slightly above 50 %. The signal from the evaporation of a test substance can be detected starting from 0.01 ng and shows a linear response in the mass spectrometer. Instrument operation in the range of pg/m3 is demonstrated by an example measurement of 15 nm particles produced by nucleation from dimethylamine, sulfuric acid and water.
In late 2013, a whole air flask collection program started at the Taunus Observatory (TO) in central Germany. Being a rural site in close vicinity to the densely populated Rhein-Main area, Taunus Observatory allows to assess local and regional emissions. Owed to its altitude of 825 m, the site also regularly experiences background conditions, especially when air masses approach from north-westerly directions. With a large footprint area mainly covering central Europe north of the Alps, halocarbon measurements at the site have the potential to improve the data base for estimation of regional and total European halogenated greenhouse gas emissions. Flask samples are collected weekly for offline analysis using a GC-MS system employing a quadrupole as well as a time-of-flight mass spectrometer. As background reference, additional samples are collected approximately bi-weekly at the Mace Head Atmospheric Research Station (MHD) when air masses approach from the site’s clean air sector. Thus the TO time series can be linked to the in-situ AGAGE measurements and the NOAA flask sampling program at MHD. An iterative baseline identification procedure separates polluted samples from baseline data. While there is good agreement of baseline mixing ratios between TO and MHD, with a larger variability of mixing ratios at the continental site, measurements at TO are regularly influenced by elevated halocarbon mixing ratios. Here, first time series are presented for CFC-11, CFC-12, HCFC-22, HFC-134a, HFC-227ea, HFC-245fa, and dichloromethane. While atmospheric mixing ratios of the CFCs decrease, they increase for the HCFC and the HFCs. Small unexpected differences between CFC-11 and CFC-12 are found with regard to the occurrence of high mixing ratio events and seasonality, although production and use of both compounds are strictly regulated by the Montreal Protocol, and therefore a similar decrease of atmospheric mixing ratios should occur. Dichloromethane, a solvent about which recently concerns have risen regarding its growing influence on stratospheric ozone depletion, does not show a significant trend with regard to both, baseline mixing ratios and the occurrence of pollution events at Taunus Observatory for the time period covered, indicating stable emissions in the regions that influence the site. An analysis of HYSPLIT trajectories reveals differences in halocarbon mixing ranges depending on air mass origin.
We present the application of Time-of-Flight Mass Spectrometry (TOF MS) for the analysis of halocarbons in the atmosphere, after cryogenic sample preconcentration and gas chromatographic separation. For the described field of application, the Quadrupole Mass Spectrometer (QP MS) is the state-of-the-art detector. This work aims at comparing two commercially available instruments, a QP MS and a TOF MS with respect to mass resolution, mass accuracy, sensitivity, measurement precision and detector linearity. Both mass spectrometers are operated on the same gas chromatographic system by splitting the column effluent to both detectors. The QP MS had to be operated in optimised Single Ion Monitoring (SIM) mode to achieve a sensitivity which could compete with the TOF MS. The TOF MS provided full mass range information in any acquired mass spectrum without losing sensitivity. Whilst the QP MS showed the performance already achieved in earlier tests, the sensitivity of the TOF MS was on average higher than that of the QP MS in the "operational" SIM mode by a factor of up to 3 reaching detection limits of less than 0.2 pg. Measurement precision determined for the whole analytical system was up to 0.2% depending on substance and sampled volume. The TOF MS instrument used for this study displayed significant non-linearities of up to 10% for two third of all analysed substances.
A new method for size-resolved chemical analysis of nucleation mode aerosol particles (size range from ∼10 to ∼30 nm) is presented. The Thermal Desorption Differential Mobility Analyzer (TD-DMA) uses an online, discontinuous principle. The particles are charged, a specific size is selected by differential mobility analysis and they are collected on a filament by electrostatic precipitation. Subsequently, the sampled mass is evaporated in a clean carrier gas and analyzed by a chemical ionization mass spectrometer. Gas-phase measurements are performed with the same mass spectrometer during the sampling of particles. The characterization shows reproducible results, with a particle size resolution of 1.19 and the transmission efficiency for 15 nm particles being slightly above 50 %. The signal from the evaporation of a test substance can be detected starting from 0.01 ng and shows a linear response in the mass spectrometer. Instrument operation in the range of pg m−3 is demonstrated by an example measurement of 15 nm particles produced by nucleation from dimethylamine, sulfuric acid and water.
In late 2013, a whole air flask collection programme was started at Taunus Observatory (TO) in central Germany. Being a rural site in close proximity to the Rhine–Main area, Taunus Observatory allows assessment of emissions from a densely populated region. Owing to its altitude of 825 m, the site also regularly experiences background conditions, especially when air masses approach from north-westerly directions. With a large footprint area mainly covering central Europe north of the Alps, halocarbon measurements at the site have the potential to improve the database for estimation of regional and total European halogenated greenhouse gas emissions. Flask samples are collected weekly for offline analysis using a GC/MS system simultaneously employing a quadrupole as well as a time-of-flight mass spectrometer. As background reference, additional samples are collected approximately once every 2 weeks at the Mace Head Atmospheric Research Station (MHD) when air masses approach from the site's clean air sector. Thus the time series at TO can be linked to the in situ AGAGE measurements and the NOAA flask sampling programme at MHD. An iterative baseline identification procedure separates polluted samples from baseline data. While there is good agreement of baseline mixing ratios between TO and MHD, with a larger variability of mixing ratios at the continental site, measurements at TO are regularly influenced by elevated halocarbon mixing ratios. Here, first time series are presented for CFC-11, CFC-12, HCFC-22, HFC-134a, HFC-227ea, HFC-245fa, and dichloromethane. While atmospheric mixing ratios of the chlorofluorocarbons (CFCs) decrease, they increase for the hydrochlorofluorocarbons (HCFCs) and the hydrofluorocarbons (HFCs). Small unexpected differences between CFC-11 and CFC-12 are found with regard to frequency and relative enhancement of high mixing ratio events and seasonality, although production and use of both compounds are strictly regulated by the Montreal Protocol, and therefore a similar decrease in atmospheric mixing ratios should occur. Dichloromethane, a solvent about which recently concerns have been raised regarding its growing influence on stratospheric ozone depletion, does not show a significant trend with regard to both baseline mixing ratios and the occurrence of pollution events at Taunus Observatory for the time period covered, indicating stable emissions in the regions that influence the site. An analysis of trajectories from the Hybrid Single Particle Lagrangian Integrated Trajectory (HYSPLIT) model reveals differences in halocarbon mixing ranges depending on air mass origin.
