Examination of Organic Vapor Adsorption onto Alkali Metal and Halide Atomic Ions by using Ion Mobility Mass Spectrometry

We utilize ion mobility mass spectrometry with an atmospheric pressure differential mobility analyzer coupled to a time‐of‐flight mass spectrometer (DMA‐MS) to examine the formation of ion‐vapor molecule complexes with seed ions of K+, Rb+, Cs+, Br−, and I− exposed to n‐butanol and n‐nonane vapor un...

Full description

Saved in:
Bibliographic Details
Published inChemphyschem Vol. 18; no. 21; pp. 3039 - 3046
Main Authors Maiβer, Anne, Hogan, Christopher J.
Format Journal Article
LanguageEnglish
Published Germany Wiley Subscription Services, Inc 03.11.2017
John Wiley and Sons Inc
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:We utilize ion mobility mass spectrometry with an atmospheric pressure differential mobility analyzer coupled to a time‐of‐flight mass spectrometer (DMA‐MS) to examine the formation of ion‐vapor molecule complexes with seed ions of K+, Rb+, Cs+, Br−, and I− exposed to n‐butanol and n‐nonane vapor under subsaturated conditions. Ion‐vapor molecule complex formation is indicated by a shift in the apparent mobility of each ion. Measurement results are compared to predicted mobility shifts based upon the Kelvin–Thomson equation, which is commonly used in predicting rates of ion‐induced nucleation. We find that n‐butanol at saturation ratios as low as 0.03 readily binds to all seed ions, leading to mobility shifts in excess of 35 %. Conversely, the binding of n‐nonane is not detectable for any ion for saturation ratios in the 0–0.27 range. An inverse correlation between the ionic radius of the initial seed and the extent of n‐butanol uptake is observed, such that at elevated n‐butanol concentrations, the smallest ion (K+) has the smallest apparent mobility and the largest (I−) has the largest apparent mobility. Though the differences in behavior of the two vapor molecules types examined and the observed effect of ionic seed radius are not accounted for by the Kelvin–Thomson equation, its predictions are in good agreement with measured mobility shifts for Rb+, Cs+, and Br− in the presence of n‐butanol (typically within 10 % of measurements). Stuck on you: Ion mobility mass spectrometry with an atmospheric pressure differential mobility analyzer is used to examine shifts in the inverse mobilities of atomic seed ions exposed to organic vapor. The observed mobility shifts are related to the adsorption of vapor molecules to ions and are compared to predictions based on the Kelvin–Thomson equation.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:1439-4235
1439-7641
DOI:10.1002/cphc.201700747