Positive Reactant Ion Formation in High Kinetic Energy Ion Mobility Spectrometry (HiKE-IMS)

Research output: Contribution to journalArticleResearchpeer review

Authors

  • Maria Allers
  • Ansgar Thomas Kirk
  • Manuel Eckermann
  • Christoph Schaefer
  • Duygu Erdogdu
  • Walter Wissdorf
  • Thorsten Benter
  • Stefan Zimmermann

External Research Organisations

  • The University of Wuppertal
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Details

Original languageEnglish
Pages (from-to)1291-1301
Number of pages11
JournalJournal of the American Society for Mass Spectrometry
Volume31
Issue number6
Early online date6 May 2020
Publication statusPublished - 3 Jun 2020

Abstract

In contrast to classical Ion Mobility Spectrometers (IMS) operating at ambient pressure, the High Kinetic Energy Ion Mobility Spectrometer (HiKE-IMS) is operated at reduced pressures of between 10 and 40 mbar and higher reduced electric field strengths of up to 120 Td. Thus, the ion-molecule reactions occurring in the HiKE-IMS can significantly differ from those in classical ambient pressure IMS. In order to predict the ionization pathways of specific analyte molecules, profound knowledge of the reactant ion species generated in HiKE-IMS and their dependence on the ionization conditions is essential. In this work, the formation of positive reactant ions in HiKE-IMS is investigated in detail. On the basis of kinetic and thermodynamic data from the literature, the ion-molecule reactions are kinetically modeled. To verify the model, we present measurements of the reactant ion population and its dependence on the reduced electric field strength, the operating pressure, and the water concentration in the sample gas. All of these parameters significantly affect the reactant ion population formed in HiKE-IMS.

Keywords

    corona discharge ionization, high kinetic energy ion mobility spectrometry, HiKE-IMS, IMS, ion mobility spectrometry, kinetic modeling, positive reactant ion formation

ASJC Scopus subject areas

Cite this

Positive Reactant Ion Formation in High Kinetic Energy Ion Mobility Spectrometry (HiKE-IMS). / Allers, Maria; Kirk, Ansgar Thomas; Eckermann, Manuel et al.
In: Journal of the American Society for Mass Spectrometry, Vol. 31, No. 6, 03.06.2020, p. 1291-1301.

Research output: Contribution to journalArticleResearchpeer review

Allers M, Kirk AT, Eckermann M, Schaefer C, Erdogdu D, Wissdorf W et al. Positive Reactant Ion Formation in High Kinetic Energy Ion Mobility Spectrometry (HiKE-IMS). Journal of the American Society for Mass Spectrometry. 2020 Jun 3;31(6):1291-1301. Epub 2020 May 6. doi: 10.1021/jasms.0c00114
Allers, Maria ; Kirk, Ansgar Thomas ; Eckermann, Manuel et al. / Positive Reactant Ion Formation in High Kinetic Energy Ion Mobility Spectrometry (HiKE-IMS). In: Journal of the American Society for Mass Spectrometry. 2020 ; Vol. 31, No. 6. pp. 1291-1301.
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abstract = "In contrast to classical Ion Mobility Spectrometers (IMS) operating at ambient pressure, the High Kinetic Energy Ion Mobility Spectrometer (HiKE-IMS) is operated at reduced pressures of between 10 and 40 mbar and higher reduced electric field strengths of up to 120 Td. Thus, the ion-molecule reactions occurring in the HiKE-IMS can significantly differ from those in classical ambient pressure IMS. In order to predict the ionization pathways of specific analyte molecules, profound knowledge of the reactant ion species generated in HiKE-IMS and their dependence on the ionization conditions is essential. In this work, the formation of positive reactant ions in HiKE-IMS is investigated in detail. On the basis of kinetic and thermodynamic data from the literature, the ion-molecule reactions are kinetically modeled. To verify the model, we present measurements of the reactant ion population and its dependence on the reduced electric field strength, the operating pressure, and the water concentration in the sample gas. All of these parameters significantly affect the reactant ion population formed in HiKE-IMS.",
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AU - Erdogdu, Duygu

AU - Wissdorf, Walter

AU - Benter, Thorsten

AU - Zimmermann, Stefan

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N2 - In contrast to classical Ion Mobility Spectrometers (IMS) operating at ambient pressure, the High Kinetic Energy Ion Mobility Spectrometer (HiKE-IMS) is operated at reduced pressures of between 10 and 40 mbar and higher reduced electric field strengths of up to 120 Td. Thus, the ion-molecule reactions occurring in the HiKE-IMS can significantly differ from those in classical ambient pressure IMS. In order to predict the ionization pathways of specific analyte molecules, profound knowledge of the reactant ion species generated in HiKE-IMS and their dependence on the ionization conditions is essential. In this work, the formation of positive reactant ions in HiKE-IMS is investigated in detail. On the basis of kinetic and thermodynamic data from the literature, the ion-molecule reactions are kinetically modeled. To verify the model, we present measurements of the reactant ion population and its dependence on the reduced electric field strength, the operating pressure, and the water concentration in the sample gas. All of these parameters significantly affect the reactant ion population formed in HiKE-IMS.

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