TY - JOUR
T1 - Laboratory characterization of furan, 2(3H)-furanone, 2-furaldehyde, 2,5-dimethylfuran, and maleic anhydride measured by PTR-ToF-MS
AU - Permar, Wade
AU - Tucker, Mercedes
AU - Hu, Lu
N1 - Publisher Copyright:
© Copyright 2025 Wade Permar et al.
PY - 2025/11/18
Y1 - 2025/11/18
N2 - Furanoids are significant contributors to volatile organic compound hydroxyl radical reactivity in biomass burning emissions, yet their accurate measurement using proton-transfer-reaction time-of-flight mass spectrometry (PTR-ToF-MS) remains challenging due to potential interferences and measurement uncertainties. In this study, we conduct detailed laboratory characterizations of furan (C4H4O, protonated m/z 69.033), 2(3H)-furanone (C4H4O2, m/z 85.028), 2-furaldehyde (C5H4O2, m/z 97.028), 2,5-dimethylfuran (C6H8O, m/z 97.065), and maleic anhydride (C4H2O3, m/z 99.008). Sensitivities for these compounds were found to have minimal dependence (less than 15 %) on both sample humidity and drift tube electric field strength (E/N). At high E/N (150 Td), fragmentation was observed for 2-furaldehyde (∼ 8 %) at m/z 69.033, potentially interfering furan measurements, while hydrolysis products corresponding to m/z+18 ions were detected for 2(3H)-furanone, 2-furaldehyde, and maleic anhydride. The hydrolysis of maleic anhydride to maleic acid is most prominent, with the hydrate accounting for 7 %-31 % of the parent ion signal across E/N conditions. Gas standard recertification confirmed the long-term stability of furanoids, and 21 other VOCs, in compressed gas mixtures, with changes in mixing ratios of less than 5 % over seven years, although PTR-ToF-MS instrument sensitivities decreased by ∼ 30 % during this time, likely due to aging of the microchannel plate (MCP). While the stability of gas standards and the minimal humidity and fragmentation effects support the accurate measurement of furanoids by PTR-ToF-MS, discrepancies with co-deployed gas chromatography-mass spectrometry highlight the need to further investigate potential isomeric and fragment interferences, particularly in aged BB smoke.
AB - Furanoids are significant contributors to volatile organic compound hydroxyl radical reactivity in biomass burning emissions, yet their accurate measurement using proton-transfer-reaction time-of-flight mass spectrometry (PTR-ToF-MS) remains challenging due to potential interferences and measurement uncertainties. In this study, we conduct detailed laboratory characterizations of furan (C4H4O, protonated m/z 69.033), 2(3H)-furanone (C4H4O2, m/z 85.028), 2-furaldehyde (C5H4O2, m/z 97.028), 2,5-dimethylfuran (C6H8O, m/z 97.065), and maleic anhydride (C4H2O3, m/z 99.008). Sensitivities for these compounds were found to have minimal dependence (less than 15 %) on both sample humidity and drift tube electric field strength (E/N). At high E/N (150 Td), fragmentation was observed for 2-furaldehyde (∼ 8 %) at m/z 69.033, potentially interfering furan measurements, while hydrolysis products corresponding to m/z+18 ions were detected for 2(3H)-furanone, 2-furaldehyde, and maleic anhydride. The hydrolysis of maleic anhydride to maleic acid is most prominent, with the hydrate accounting for 7 %-31 % of the parent ion signal across E/N conditions. Gas standard recertification confirmed the long-term stability of furanoids, and 21 other VOCs, in compressed gas mixtures, with changes in mixing ratios of less than 5 % over seven years, although PTR-ToF-MS instrument sensitivities decreased by ∼ 30 % during this time, likely due to aging of the microchannel plate (MCP). While the stability of gas standards and the minimal humidity and fragmentation effects support the accurate measurement of furanoids by PTR-ToF-MS, discrepancies with co-deployed gas chromatography-mass spectrometry highlight the need to further investigate potential isomeric and fragment interferences, particularly in aged BB smoke.
UR - https://www.scopus.com/pages/publications/105022172580
U2 - 10.5194/amt-18-6645-2025
DO - 10.5194/amt-18-6645-2025
M3 - Article
AN - SCOPUS:105022172580
SN - 1867-1381
VL - 18
SP - 6645
EP - 6657
JO - Atmospheric Measurement Techniques
JF - Atmospheric Measurement Techniques
IS - 22
ER -