A Method for the Determination of Rate Coefficients\nfor the Formation of Protonated Monomers and Proton Bound Dimers of\nVolatile Organic Compounds in Air at Ambient Pressure by Ion Mobility\nSpectrometry

Rate coefficients\n(<i>k</i>) for the reactions of hydrated\nprotons and a sample vapor (M) to form protonated monomers (MH<sup>+</sup>(H<sub>2</sub>O)<sub><i>n</i></sub>) and proton\nbound dimers (M<sub>2</sub>H<sup>+</sup>) were determined simultaneously\nby using ion mobility spectrometry with a tandem drift tube at ambient\npressure. In this method, sample vapors were introduced to a first\ndrift region with stepwise reactions: M + H<sup>+</sup>(H<sub>2</sub>O)<i>n</i>→k1 <sub>MH</sub><sup>+</sup> (H<sub>2</sub>O)<sub><i>y</i></sub> + (<i>n</i> – <i>y</i>) H<sub>2</sub>O and M + MH<sup>+</sup> (H<sub>2</sub>O)<i>y</i>→k2 M<sub>2</sub>H<sup>+</sup> + <i>y</i>H<sub>2</sub>O. Ions with a drift time between\n9 and 18 ms in the\nfirst drift region were subsequently mobility analyzed in purified\nair with the second drift region using a synchronized second ion gate\nwith boxcar averaging. Slope for plots of ion abundance against drift\ntime was fitted by successive approximation between peaks of H<sup>+</sup>(H<sub>2</sub>O)<sub><i>n</i></sub> and MH<sup>+</sup>(H<sub>2</sub>O)<sub><i>y</i></sub> to obtain <i>k</i><sub>2</sub> until computed and experimental slopes matched within\na maximal deviation of 0.01. Values for <i>k</i><sub>1</sub> were obtained from the experimental baseline slope when adjusted\nfor <i>k</i><sub>2</sub>. Rate coefficients for triethyl\nphosphate and phenylacetate were determined using this method with <i>k</i><sub>1</sub> values of 1.14 × 10<sup>–9</sup> ± 1.87 × 10<sup>–10</sup> cm<sup>3</sup>/s and\n0.81 × 10<sup>–9</sup> ± 9.26 × 10<sup>–11</sup> cm<sup>3</sup>/s and <i>k</i><sub>2</sub> values of 1.05\n× 10<sup>–9</sup> ± 4.13 × 10<sup>–10</sup> cm<sup>3</sup>/s and 1.07 × 10<sup>–9</sup> ± 1.86\n× 10<sup>–10</sup> cm<sup>3</sup>/s, respectively. Relative\nerror for this method was determined using mobility spectra generated\nwith a COMSOL model and artificial rate coefficients. Rate coefficients\nwere then extracted from the modeled mobility spectra and compared\nto the original artificial values. Relative error of this method was\n10% and should be generally applicable for individual substances with\nreactions forming protonated monomers and proton bound dimers.

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2024-12-04
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https://doi.org/10.1021/acs.analchem.4c04434.s001
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Mass Spectrometry Techniques and Applications
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article

A Method for the Determination of Rate Coefficients\nfor the Formation of Protonated Monomers and Proton Bound Dimers of\nVolatile Organic Compounds in Air at Ambient Pressure by Ion Mobility\nSpectrometry

Figshare
Mass Spectrometry Techniques and Applications
article

A Method for the Determination of Rate Coefficients\nfor the Formation of Protonated Monomers and Proton Bound Dimers of\nVolatile Organic Compounds in Air at Ambient Pressure by Ion Mobility\nSpectrometry

article en

Abstract

Rate coefficients\n(<i>k</i>) for the reactions of hydrated\nprotons and a sample vapor (M) to form protonated monomers (MH<sup>+</sup>(H<sub>2</sub>O)<sub><i>n</i></sub>) and proton\nbound dimers (M<sub>2</sub>H<sup>+</sup>) were determined simultaneously\nby using ion mobility spectrometry with a tandem drift tube at ambient\npressure. In this method, sample vapors were introduced to a first\ndrift region with stepwise reactions: M + H<sup>+</sup>(H<sub>2</sub>O)<i>n</i>→k1 <sub>MH</sub><sup>+</sup> (H<sub>2</sub>O)<sub><i>y</i></sub> + (<i>n</i> – <i>y</i>) H<sub>2</sub>O and M + MH<sup>+</sup> (H<sub>2</sub>O)<i>y</i>→k2 M<sub>2</sub>H<sup>+</sup> + <i>y</i>H<sub>2</sub>O. Ions with a drift time between\n9 and 18 ms in the\nfirst drift region were subsequently mobility analyzed in purified\nair with the second drift region using a synchronized second ion gate\nwith boxcar averaging. Slope for plots of ion abundance against drift\ntime was fitted by successive approximation between peaks of H<sup>+</sup>(H<sub>2</sub>O)<sub><i>n</i></sub> and MH<sup>+</sup>(H<sub>2</sub>O)<sub><i>y</i></sub> to obtain <i>k</i><sub>2</sub> until computed and experimental slopes matched within\na maximal deviation of 0.01. Values for <i>k</i><sub>1</sub> were obtained from the experimental baseline slope when adjusted\nfor <i>k</i><sub>2</sub>. Rate coefficients for triethyl\nphosphate and phenylacetate were determined using this method with <i>k</i><sub>1</sub> values of 1.14 × 10<sup>–9</sup> ± 1.87 × 10<sup>–10</sup> cm<sup>3</sup>/s and\n0.81 × 10<sup>–9</sup> ± 9.26 × 10<sup>–11</sup> cm<sup>3</sup>/s and <i>k</i><sub>2</sub> values of 1.05\n× 10<sup>–9</sup> ± 4.13 × 10<sup>–10</sup> cm<sup>3</sup>/s and 1.07 × 10<sup>–9</sup> ± 1.86\n× 10<sup>–10</sup> cm<sup>3</sup>/s, respectively. Relative\nerror for this method was determined using mobility spectra generated\nwith a COMSOL model and artificial rate coefficients. Rate coefficients\nwere then extracted from the modeled mobility spectra and compared\nto the original artificial values. Relative error of this method was\n10% and should be generally applicable for individual substances with\nreactions forming protonated monomers and proton bound dimers.

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