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Published September 1, 2021 | Published + Supplemental Material
Journal Article Open

Molecular characterization of ultrafine particles using extractive electrospray time-of-flight mass spectrometry

Abstract

Aerosol particles negatively affect human health while also having climatic relevance due to, for example, their ability to act as cloud condensation nuclei. Ultrafine particles (diameter D_p < 100 nm) typically comprise the largest fraction of the total number concentration, however, their chemical characterization is difficult because of their low mass. Using an extractive electrospray time-of-flight mass spectrometer (EESI-TOF), we characterize the molecular composition of freshly nucleated particles from naphthalene and β-caryophyllene oxidation products at the CLOUD chamber at CERN. We perform a detailed intercomparison of the organic aerosol chemical composition measured by the EESI-TOF and an iodide adduct chemical ionization mass spectrometer equipped with a filter inlet for gases and aerosols (FIGAERO-I-CIMS). We also use an aerosol growth model based on the condensation of organic vapors to show that the chemical composition measured by the EESI-TOF is consistent with the expected condensed oxidation products. This agreement could be further improved by constraining the EESI-TOF compound-specific sensitivity or considering condensed-phase processes. Our results show that the EESI-TOF can obtain the chemical composition of particles as small as 20 nm in diameter with mass loadings as low as hundreds of ng m⁻³ in real time. This was until now difficult to achieve, as other online instruments are often limited by size cutoffs, ionization/thermal fragmentation and/or semi-continuous sampling. Using real-time simultaneous gas- and particle-phase data, we discuss the condensation of naphthalene oxidation products on a molecular level.

Additional Information

© 2021 The Author(s). Published by the Royal Society of Chemistry. This article is licensed under a Creative Commons Attribution-NonCommercial 3.0 Unported Licence. Submitted 26 Jun 2021; Accepted 10 Aug 2021; First published 23 Aug 2021. We thank the European Organization for Nuclear Research (CERN) for supporting CLOUD with important technical and financial resources. We would also like to thank P. Carrie, L.-P. De Menezes, F. Josa, I. Krasin, O. S. Maksumov, I. Krasin, R. Sitals and A. Wasem for their contribution to the experiment. This research has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement no. 895875 ("NPF-PANDA"), no. 764991 ("CLOUD-MOTION H2020-MSCA-ITN-2017"), Swiss National Science Foundation (grant numbers 200021_169090, 200020_172602 and 20FI20_172622), the US National Science Foundation (NSF-AGS-1649147, NSF-AGS-1801574, NSF-AGS-1801897, NSF-AGS-1531284 NSF 1602086, NSF 1801329), the Wallace Research Foundation, the NASA graduate fellowship (NASA-NNX16AP36H), the Portuguese Foundation for Science and Technology (CERN/FIS-COM/0014/2017) as well as the ERC Consolidator Grant "NANODYNAMITE" (No. 616075). We acknowledge the following projects: ACCC Flagship funded by the Academy of Finland (grant no. 337549), Academy professorship funded by the Academy of Finland (grant no. 302958), Academy of Finland projects no. 1325656, 316114 and 325647, "Quantifying carbon sink, CarbonSink+ and their interaction with air quality" INAR project funded by Jane and Aatos Erkko Foundation, European Research Council (ERC) project ATM-GTP Contract No. 742206. Author contributions: V. P., M. X., M. W., B. M., M. Sim., D. S., C. R. H., F. L.-H., L. R. A., A. A., A. B., L. D., J. Dup., C. K., J. K., K. L., V. M., B. M., U. M., W. N., L. L. J. Q., C. T., A. T., P. M. W. collected the data. V. P., M. X., M. W., B. M., M. Sim., D. S., C. R. H., F. L.-H., A. B., U. B., D. C., L. D., J. Dup., H. F., R. C. F., X.-C. H., V. H., C. K., J. K., A. Kür., A. Kvas., K. L., V. M., B. M., U. M., T. P., L. L. J. Q., A. T., R. W., P. M. W., C. Y., I. E.-H. prepared the CLOUD facility or measuring instruments. M. Sur., V. P., M. X., M. W., B. M., M. Sim., D. S., C. K., U. M. analyzed the data. M. Sur., V. P., M. X., M. W., D. S., D. M. B., C. P. L., H. L., H. F., U. M., J. K., M. Sim., D. R. W., A. S. H., J. Dup, J. Dom., N. M. D., A. H., J. C., M. K., R. C. F., R. V., J. G. S., D. S. W., U. B., I. E.-H. contributed to the scientific discussion and interpretation of results. M. Sur., V. P., J. Dom., D. S. W., U. B., I. E.-H. participated in writing the manuscript. There are no conflicts to declare.

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Additional details

Created:
August 20, 2023
Modified:
October 23, 2023