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dc.date.accessioned2022-03-26T16:15:48Z
dc.date.available2022-03-26T16:15:48Z
dc.date.created2022-02-10T13:51:04Z
dc.date.issued2021
dc.identifier.citationPiel, Felix Müller, Markus Winkler, Klaus Skytte Af Sätra, Jenny Marie Wisthaler, Armin . Introducing the extended volatility range proton-Transfer-reaction mass spectrometer (EVR PTR-MS). Atmospheric Measurement Techniques. 2021, 14(2), 1355-1363
dc.identifier.urihttp://hdl.handle.net/10852/92962
dc.description.abstractProton-transfer-reaction mass spectrometry (PTR-MS) is widely used in atmospheric sciences for measuring volatile organic compounds in real time. In the most widely used type of PTR-MS instruments, air is directly introduced into a chemical ionization reactor via an inlet capillary system. The reactor has a volumetric exchange time of ∼0.1 s, enabling PTR-MS analyzers to measure at a frequency of 10 Hz. The time response does, however, deteriorate if low-volatility analytes interact with surfaces in the inlet or in the instrument. Herein, we present the extended volatility range (EVR) PTR-MS instrument which mitigates this issue. In the EVR configuration, inlet capillaries are made of passivated stainless steel, and all wetted metal parts in the chemical ionization reactor are surface-passivated with a functionalized hydrogenated amorphous silicon coating. Heating the entire setup (up to 120 ∘C) further improves the time-response performance. We carried out time-response performance tests on a set of 29 analytes having saturation mass concentrations C0 in the range between 10−3 and 105 µg m−3. The 1/e-signal decay times after instant removal of the analyte from the sampling flow were between 0.2 and 90 s for gaseous analytes. We also tested the EVR PTR-MS instrument in combination with the chemical analysis of aerosols online (CHARON) particle inlet, and 1/e-signal decay times were in the range between 5 and 35 s for particulate analytes. We show on a set of example compounds that the time-response performance of the EVR PTR-MS instrument is comparable to that of the fastest flow tube chemical ionization mass spectrometers that are currently in use. The fast time response can be used for rapid (∼1 min equilibration time) switching between gas and particle measurements. The CHARON EVR PTR-MS instrument can thus be used for real-time monitoring of both gaseous and particulate organics in the atmosphere. Finally, we show that the CHARON EVR PTR-MS instrument also rapidly detects highly oxygenated species (with up to eight oxygen atoms) in particles formed by limonene ozonolysis.
dc.languageEN
dc.publisherCopernicus GmbH
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleIntroducing the extended volatility range proton-Transfer-reaction mass spectrometer (EVR PTR-MS)
dc.typeJournal article
dc.creator.authorPiel, Felix
dc.creator.authorMüller, Markus
dc.creator.authorWinkler, Klaus
dc.creator.authorSkytte Af Sätra, Jenny Marie
dc.creator.authorWisthaler, Armin
cristin.unitcode185,15,12,0
cristin.unitnameKjemisk institutt
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.cristin2000003
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Atmospheric Measurement Techniques&rft.volume=14&rft.spage=1355&rft.date=2021
dc.identifier.jtitleAtmospheric Measurement Techniques
dc.identifier.volume14
dc.identifier.issue2
dc.identifier.startpage1355
dc.identifier.endpage1363
dc.identifier.doihttps://doi.org/10.5194/amt-14-1355-2021
dc.identifier.urnURN:NBN:no-95554
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn1867-1381
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/92962/1/amt-14-1355-2021.pdf
dc.type.versionPublishedVersion
dc.relation.projectEC/H2020/674911
dc.relation.projectEC/H2020/65410


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