Please use this identifier to cite or link to this item: https://doi.org/10.5194/amt-6-3211-2013
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dc.titleHigh-resolution chemical ionization mass spectrometry (ToF-CIMS): Application to study SOA composition and processing
dc.contributor.authorAljawhary, D
dc.contributor.authorLee, A.K.Y
dc.contributor.authorAbbatt, J.P.D
dc.date.accessioned2020-11-10T00:29:07Z
dc.date.available2020-11-10T00:29:07Z
dc.date.issued2013
dc.identifier.citationAljawhary, D, Lee, A.K.Y, Abbatt, J.P.D (2013). High-resolution chemical ionization mass spectrometry (ToF-CIMS): Application to study SOA composition and processing. Atmospheric Measurement Techniques 6 (11) : 3211-3224. ScholarBank@NUS Repository. https://doi.org/10.5194/amt-6-3211-2013
dc.identifier.issn18671381
dc.identifier.urihttps://scholarbank.nus.edu.sg/handle/10635/183191
dc.description.abstractThis paper demonstrates the capabilities of chemical ionization mass spectrometry (CIMS) to study secondary organic aerosol (SOA) composition with a high-resolution (HR) time-of-flight mass analyzer (aerosol-ToF-CIMS). In particular, by studying aqueous oxidation of water-soluble organic compounds (WSOC) extracted from ?-pinene ozonolysis SOA, we assess the capabilities of three common CIMS reagent ions: (a) protonated water clusters (H 2O)nH+, (b) acetate CH3C(O)O- and (c) iodide water clusters I(H2O)n- to monitor SOA composition. Furthermore, we report the relative sensitivity of these reagent ions to a wide range of common organic aerosol constituents. We find that (H2O)nH+ is more selective to the detection of less oxidized species, so that the range of O / C and OSC (carbon oxidation state) in the SOA spectra is considerably lower than those measured using CH3C(O)O- and I(H2O)n - Specifically, (H2O)nH+ ionizes organic compounds with OSC ≤ 1.3, whereas CH3C(O)O- and I(H 2O)n- both ionize highly oxygenated organics with OSC up to 4 with I(H2O)n- being more selective towards multi-functional organic compounds. In the bulk O / C and H / C space (in a Van Krevelen plot), there is a remarkable agreement in both absolute magnitude and oxidation trajectory between ToF-CIMS data and those from a high-resolution aerosol mass spectrometer (HR-AMS). Despite not using a sensitivity-weighted response for the ToF-CIMS data, the CIMS approach appears to capture much of the chemical change occurring. As demonstrated by the calibration experiments with standards, this is likely because there is not a large variability in sensitivities from one highly oxygenated species to another, particularly for the CH3- and I(H2O)n- reagent ions. Finally, the data illustrate the capability of aerosol-ToF-CIMS to monitor specific chemical change, including the fragmentation and functionalization reactions that occur during organic oxidation, and the oxidative conversion of dimeric SOA species into monomers. Overall, aerosol-ToF-CIMS is a valuable, selective complement to some common SOA characterization methods, such as AMS and spectroscopic techniques. Both laboratory and ambient SOA samples can be analyzed using the techniques illustrated in the paper. © 2013 Author(s).f 0.
dc.rightsAttribution 4.0 International
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.sourceUnpaywall 20201031
dc.subjectaerosol composition
dc.subjectdata set
dc.subjectdetection method
dc.subjectmass spectrometry
dc.subjectoxidation
dc.subjectozone
dc.typeArticle
dc.contributor.departmentCIVIL AND ENVIRONMENTAL ENGINEERING
dc.description.doi10.5194/amt-6-3211-2013
dc.description.sourcetitleAtmospheric Measurement Techniques
dc.description.volume6
dc.description.issue11
dc.description.page3211-3224
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