Vocus PTR-TOF mass spectra are dominated by protonated peaks and free of significant contributions from non-PTR reaction and therefore easily interpreted and quantified.
Felipe Lopez-Hilfiker, Liang Zhu, Manuel Hutterli, Luca Cappellin
TOFWERK, Thun, Switzerland
Online CI-MS Analysis of Air Demands Well Understood Ion Chemistry
Air samples that contain volatile organic compounds (VOCs) are often complex mixtures of tens or hundreds of different trace compounds. Traditional techniques for analysis of such samples require labor-intensive sample preparation and chromatographic separation, thus limiting measurement throughput and/or the time resolution of the VOC measurements. In contrast, chemical ionization mass spectrometry (CI-MS) can quantitatively measure VOCs in real-time with sub-second time resolution. These fast, online capabilities stem from easy-to-understand ion chemistry that allows ionization and mass spectral detection of VOCs without the need for sample preparation or chromatographic separation.
In CI-MS, air that contains neutral, gas-phase analyte molecules is directly sampled into the mass spectrometer. Analyte molecules are ionized by way of chemical reactions with high-concentration reactant ions (aka primary ions or reagent ions) under controlled conditions. The analyte ions produced in these reactions are subsequently measured by a mass analyzer, which determines the ions’ mass/charge values and abundances. The level of difficulty of interpreting the mass spectrum depends on the complexity of the ion chemistry – which is largely determined by the reagent ion of choice – and the purity of the ion source. For a given ion chemistry, the purer the source of reactant ions, the easier the spectrum is to interpret.
High Purity Reactant Ions Make Vocus Data Readily Interpretable
Proton transfer reaction mass spectrometry (PTR-MS) is a type of CI-MS that is widely used for online detection of VOCs. The Vocus PTR-TOF is an ultra-sensitive PTR-MS that combines TOFWERK’s proprietary Vocus reactor technology and a time-of-flight mass analyzer. High abundance H3O+ reactant ions are produced with water vapor in a low-pressure plasma in a dedicated ion source region. The generated reactant ions transferred into a recombination region before entering the ion-molecule reaction region where H3O+ ions transfer protons to neutral VOC analyte molecules, creating VOC analyte ions that can be measured by the mass analyzer.
In practice, PTR mass spectra can be corrupted by spectral peaks originating from parasitic reactant ions (e.g., NO+, O2+), generated from either back-diffusion of air into the primary plasma region or the reaction of excited radicals exiting the ion source and meeting the sample flow. The presence of spurious O2+ and NO+ ions complicate the spectrum because both are capable of ionizing common VOCs via charge transfer pathways to yield different (non-protonated) product ions or driving fragmentation reactions.
The purity of the reagent ion source used for PTR-MS can be determined by either a) direct comparison of O2+ and NO+ signal to that of H3O+ or b) the ratio of the protonated and non-protonated signals of targeted compounds. The latter approach better reflects the reaction conditions in the IMR as additional quenching time during transit through the reactor can distort the actual reactor conditions and the observed relative abundances of H3O+, O2+, and NO+.
Figure 1 compares protonated to non-protonated peaks in Vocus PTR-TOF data for a series of VOCs of varied mass/charge and having different functional groups. In all cases, the VOCs are charged predominantly by protonation, with only minor contributions (~1-3%) from spurious charge transfer reactions, demonstrating the high purity of the Vocus ion source. At this high purity, Vocus mass spectra are dominated by protonated peaks and free of significant contributions from non-PTR reaction and therefore easily interpreted and quantified.