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 "title": "Proton-transfer-reaction mass spectrometry",
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 "excerpt": "Proton-transfer-reaction mass spectrometry (PTR-MS) is an analytical technique that ionizes trace volatile organic compounds directly in air using hydronium ions, introduced in 1995 and used in breath analysis and atmospheric monitoring.",
 "snippet": "Proton-transfer-reaction mass spectrometry (PTR-MS) is an analytical technique that ionizes trace volatile organic compounds directly in air using hydronium ions, introduced in 1995 and used in breath analysis and atmospheric monitoring.",
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 "markdown": "# Proton-transfer-reaction mass spectrometry\n\nProton-transfer-reaction mass spectrometry (PTR-MS) is an analytical technique that ionizes trace volatile organic compounds (VOCs) directly in air using hydronium ions and detects them by mass spectrometry, providing real-time, on-line measurements.<sup>[1](https://www.nature.com/articles/s42254-026-00990-1)</sup> Ambient air is sampled continuously into a reactor held at a few mbar, where trace gases are ionized by proton transfer with \\( H_{3} \\)O⁺ and its water clusters, without preconcentration or removal of ozone or water.<sup>[2](https://actris.eu/sites/default/files/inline-files/PTRMS%20SOP%20%28April2025%29.pdf)</sup> Full analyses take from 100 ms to a few seconds depending on the number of target compounds and the mass analyzer in use.<sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup>\n\n| Key fact | Value |\n|---|---|\n| Core reaction | \\( H_{3} \\)O⁺ + M → MH⁺ + \\( H_{2} \\)O, favorable when the proton affinity of M exceeds that of water (691 kJ/mol)<sup>[2](https://actris.eu/sites/default/files/inline-files/PTRMS%20SOP%20%28April2025%29.pdf)</sup> |\n| Detection limits | Low pptv for commercial PTR-ToF-MS, with a linear range over more than 6 orders of magnitude<sup>[4](https://pmc.ncbi.nlm.nih.gov/articles/PMC5838793/)</sup> |\n| Time resolution | 100 ms to a few seconds per full analysis; up to 10 Hz<sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup><sup> • </sup><sup>[2](https://actris.eu/sites/default/files/inline-files/PTRMS%20SOP%20%28April2025%29.pdf)</sup> |\n| Standard operating window | 1–4 mbar, 30–120 °C, E/N of 100–160 Td<sup>[5](https://amt.copernicus.org/articles/12/6193/2019/amt-12-6193-2019.pdf)</sup> |\n| Calibration-free accuracy | Better than ±30% for uncalibrated organics when simple reaction kinetics hold<sup>[5](https://amt.copernicus.org/articles/12/6193/2019/amt-12-6193-2019.pdf)</sup> |\n| Mass resolving power (ToF) | 1,000–10,000 m/Δm<sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup> |\n| Main applications | Breath analysis, food and flavor science, atmospheric VOC fluxes, indoor air<sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup> |\n\n## How it works\n\nA discharge in a water-vapor flow generates \\( H_{3} \\)O⁺ reagent ions, which encounter analyte molecules (M) from the sampled air in the drift tube according to \\( H_{3} \\)O⁺ + M → MH⁺ + \\( H_{2} \\)O.<sup>[1](https://www.nature.com/articles/s42254-026-00990-1)</sup> The reaction is thermochemically favorable when the [proton affinity](https://www.edgepedia.org/proton-affinity) of M exceeds that of water. The major air constituents (\\( N_{2} \\), \\( O_{2} \\), Ar, CO₂, CH₄) have proton affinities below that of water and remain largely silent, so ambient air can serve as the buffer gas and absolute quantification is possible without continuous gas standards.<sup>[1](https://www.nature.com/articles/s42254-026-00990-1)</sup><sup> • </sup><sup>[6](https://www.ionicon.com/technologies/details/ptr-ms)</sup>\n\n[Soft ionization](https://www.edgepedia.org/soft-ionization) is the second key property. Ionizing hydrocarbons by electron impact fragments them extensively, whereas proton transfer of \\( H_{3} \\)O⁺ to a molecule whose proton affinity is only slightly above that of water avoids this fragmentation.<sup>[7](https://www.osti.gov/etdeweb/servlets/purl/20020157)</sup> Most organics therefore appear as the protonated molecular ion MH⁺, which is what makes real-time, compound-specific monitoring practical.\n\n## How it is done\n\nThe instrument has three main parts: the ion source where \\( H_{3} \\)O⁺ is produced, the drift tube where sample air is introduced and analytes are ionized, and the mass detector where the ion signal is generated.<sup>[8](https://www.osti.gov/servlets/purl/1251396)</sup> In the usual configuration, a hollow-cathode discharge in water vapor creates \\( H_{3} \\)O⁺ reagent ions in an external ion source; these are injected into a drift tube held at reduced pressure, typically around 2 mbar, and mixed with the sample gas.<sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup>\n\nAn axial electric field in the drift tube raises ion kinetic energy and suppresses clustering of reagent and product ions with water.<sup>[9](https://www.sciencedirect.com/science/article/abs/pii/S1387380602009260)</sup> Below about 100–120 Td, water clusters of hydronium build up: the (\\( H_{2} \\)O)\\( H_{3} \\)O⁺ cluster can exceed 10% of primary ion counts, sensitivities drop by up to 50% for some compounds, and modified concentration formulas are needed.<sup>[4](https://pmc.ncbi.nlm.nih.gov/articles/PMC5838793/)</sup><sup> • </sup><sup>[5](https://amt.copernicus.org/articles/12/6193/2019/amt-12-6193-2019.pdf)</sup>\n\nQuantification without calibration rests on the reaction kinetics. The product-ion count rate follows\n\n\\[ i(\\mathrm{MH^+}) = i(\\mathrm{H_3O^+})\\left(1 - e^{-k[\\mathrm{M}]t}\\right) \\approx i(\\mathrm{H_3O^+})\\,k[\\mathrm{M}]\\,t, \\]\n\nwhere t is the drift-tube residence time (typically 100 µs) and k the proton-transfer rate constant (typically \\( 2 \\times 10^{-9} \\) cm³ molecule⁻¹ s⁻¹).<sup>[10](https://acp.copernicus.org/articles/8/273/2008/acp-8-273-2008.pdf)</sup> With artifacts ruled out, this kinetic approach retrieves volume mixing ratios, including for compounds with no calibration standard, to better than ±30%; published intercomparisons with other methods agree within 1–20%, and direct calibration improves accuracy to better than 10%.<sup>[5](https://amt.copernicus.org/articles/12/6193/2019/amt-12-6193-2019.pdf)</sup><sup> • </sup><sup>[8](https://www.osti.gov/servlets/purl/1251396)</sup> In practice, calibrations use gas standards: the ACTRIS protocol specifies an SI-traceable 20-compound standard covering 33–672 Da at about 1 ppmv, diluted to a few ppbv, with 30–90% relative humidity and transmission calibrated at the lowest humidity.<sup>[2](https://actris.eu/sites/default/files/inline-files/PTRMS%20SOP%20%28April2025%29.pdf)</sup> Ion purity matters: \\( H_{3} \\)O⁺ must constitute at least 80% of reagent ions, with impurities (\\( O_{2} \\)⁺, NO⁺, NH₄⁺) below 3% of the hydronium signal.<sup>[2](https://actris.eu/sites/default/files/inline-files/PTRMS%20SOP%20%28April2025%29.pdf)</sup>\n\n## Origin\n\nPTR-MS was reported by more than one group as it matured, but the introducing paper is A. Hansel and colleagues, \"Proton transfer reaction mass spectrometry: on-line trace gas analysis at the ppb level\", published in the International Journal of Mass Spectrometry and Ion Processes in 1995.<sup>[11](https://doi.org/10.1016/0168-1176%2895%2904294-u)</sup> The work was carried out at the Institut für Ionenphysik of the University of Innsbruck, and the technique has been commercialized by IONICON Analytik since 1998.<sup>[6](https://www.ionicon.com/technologies/details/ptr-ms)</sup>\n\nThe method built on earlier ion–neutral reaction work: the flowing afterglow technique, whose flow-drift-tube approach the [Innsbruck](https://www.edgepedia.org/innsbruck) apparatus adopted, and the selected ion flow tube (SIFT).<sup>[12](https://doi.org/10.1016/s0065-2199%2808%2960154-2)</sup><sup> • </sup><sup>[13](https://doi.org/10.1016/0020-7381%2876%2980133-7)</sup><sup> • </sup><sup>[7](https://www.osti.gov/etdeweb/servlets/purl/20020157)</sup> A review in Chemical Society Reviews consolidated the pptv-level capability,<sup>[14](https://pubs.rsc.org/en/content/articlelanding/1998/cs/a827347z)</sup> On-line measurements down to a few pptv were demonstrated, including on-line VOC data from aircraft flights.<sup>[15](https://iopscience.iop.org/article/10.1088/0963-0252/8/2/314)</sup>\n\n## Variants\n\nEarly instruments used quadrupole mass filters. Robert S. Blake and colleagues demonstrated proton-transfer-reaction time-of-flight mass spectrometry in 2004,<sup>[16](https://doi.org/10.1021/ac0498260)</sup> and Martin Graus, Markus Müller, and Armin Hansel reported high-resolution PTR-TOF with full mass-spectrum acquisition in 2010, with mass resolving power of 1,000–10,000 that distinguishes isobaric species.<sup>[17](https://doi.org/10.1016/j.jasms.2010.02.006)</sup><sup> • </sup><sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup>\n\nSwitchable reagent ion capability (PTR+SRI-MS), reported by A. Jordan and colleagues in 2009, adds NO⁺, \\( O_{2} \\)⁺, NH₄⁺, Kr⁺, and Xe⁺ reagent ions, enabling real-time separation of isomeric compounds.<sup>[18](https://doi.org/10.1016/j.ijms.2009.06.006)</sup><sup> • </sup><sup>[6](https://www.ionicon.com/technologies/details/ptr-ms)</sup> The Vocus, evaluated by Jordan Krechmer and colleagues in 2018, introduced a focusing ion–molecule reactor (FIMR) with a new reagent-ion source.<sup>[19](https://doi.org/10.1021/acs.analchem.8b02641)</sup> A separate adduct ionization mechanism (AIM) reactor supports positive and negative reagent ions (\\( C_{6} \\)\\( H_{6} \\)⁺, acetone dimer, NH₄⁺; Cl⁻, Br⁻, I⁻, NO₃⁻), is largely humidity-independent, and reaches parts-per-quadrillion detection limits at time resolutions up to 50 Hz, complementing PTR-MS for low-proton-affinity compounds.<sup>[20](https://www.mdpi.com/1420-3049/31/3/402)</sup> A compact PTR-ToF-MS designed for airborne use was reported by M. Müller and colleagues in 2014.<sup>[21](https://doi.org/10.5194/amt-7-3763-2014)</sup>\n\n## Applications\n\nSome of the earliest applications targeted exhaled breath analysis for disease diagnosis. Human breath contains about 30 volatile organic components above 1 ppb, with the most abundant (methanol, ethanol, acetone, propanol, isoprene) at 100–2000 ppb, and PTR-MS resolved fast metabolic processes such as the conversion of isopropanol into acetone within minutes.<sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup><sup> • </sup><sup>[7](https://www.osti.gov/etdeweb/servlets/purl/20020157)</sup> [Food science](https://www.edgepedia.org/food-science) uses PTR-MS for headspace fingerprinting of dairy, apples, chocolate, coffee, and beer, and for detecting food fraud in spices.<sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup> In atmospheric chemistry, PTR-MS measures biogenic VOC fluxes by eddy covariance and urban VOC concentrations; the 1999 aircraft work marked its entry into airborne studies.<sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup><sup> • </sup><sup>[15](https://iopscience.iop.org/article/10.1088/0963-0252/8/2/314)</sup> Indoor air is a growing area: NO⁺ chemical ionization on PTR-MS distinguishes aldehyde and ketone isomers in real time, since aldehydes react via hydride abstraction to form (M–H)⁺ ions while ketones undergo association reactions producing (M·NO)⁺ ions.<sup>[22](https://pubs.acs.org/doi/10.1021/acs.est.5c14145)</sup> The ACTRIS network issued PTR-MS measurement guidelines in April 2025.<sup>[2](https://actris.eu/sites/default/files/inline-files/PTRMS%20SOP%20%28April2025%29.pdf)</sup>\n\n## Limitations and alternatives\n\nHumidity affects responses because ionization efficiency, clustering, and fragmentation depend on molecular structure, humidity, and E/N, so targets should be calibrated under representative conditions.<sup>[1](https://www.nature.com/articles/s42254-026-00990-1)</sup> Compounds with proton affinities close to that of water are the hardest cases: formaldehyde (PA 713 kJ/mol) is difficult to quantify because of humidity-dependent deprotonation and possible bias from methanol and ethanol fragments at m/z 31.018, and alcohols lose signal because protonated analytes dehydrate.<sup>[2](https://actris.eu/sites/default/files/inline-files/PTRMS%20SOP%20%28April2025%29.pdf)</sup> [Hydrogen sulfide](https://www.edgepedia.org/hydrogen-sulfide) and phosphine are similarly difficult.<sup>[23](https://gcms.cz/labrulez-bucket-strapi-h3hsga3/application::paper.paper/syft_techcom_ptrms.pdf)</sup>\n\nFragmentation is a second failure mode. Under typical conditions (E/N = 120–150 Td), aldehydes ionized by \\( H_{3} \\)O⁺ fragment heavily, with the protonated ion [M+H]⁺ as low as 6–9% of product ions for C5–C8 compounds.<sup>[4](https://pmc.ncbi.nlm.nih.gov/articles/PMC5838793/)</sup> Isobaric and isomeric interferences are the third: without chromatography, standard PTR-MS cannot separate isomeric compounds even with high-resolution ToF-MS.<sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup> Known interferences include isoprene (m/z 69.070) from cycloalkanes and higher aldehydes, benzene signals from ethylbenzene and benzaldehyde fragments, and toluene signals from higher aromatics and monoterpenes.<sup>[2](https://actris.eu/sites/default/files/inline-files/PTRMS%20SOP%20%28April2025%29.pdf)</sup> In an indoor test-house study, confounding contributions at single m/z values ranged from 0% (ethanol, siloxanes) to 98% (at C5H9+).<sup>[24](https://pubs.rsc.org/en/content/articlehtml/2025/em/d4em00602j)</sup> Gas-chromatography pre-separation is the standard remedy; fast integrated GC interfaced with PTR-MS achieves runs within about a minute, though with weaker separation than conventional GC.<sup>[3](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)</sup> A 2025 interlaboratory method quantified product ion distributions for nearly 100 VOCs across seven laboratories using Vocus instruments, finding that E/N, ion optic voltage gradients, and quadrupole settings most strongly affect product ion distributions, and a public PID library is now available.<sup>[25](https://amt.copernicus.org/articles/18/1013/2025/)</sup>\n\nCompared with SIFT-MS, PTR-MS reagent ions are not mass-selected and not at thermal energies, so there is no generic database of rate coefficients and branching ratios and calibration standards must be run for most quantitation; SIFT-MS, which mass-selects three thermal reagent ions (\\( H_{3} \\)O⁺, NO⁺, \\( O_{2} \\)⁺), offers an advantage in discriminating isomers and in calibration-free absolute quantitation.<sup>[23](https://gcms.cz/labrulez-bucket-strapi-h3hsga3/application::paper.paper/syft_techcom_ptrms.pdf)</sup>\n\n## References\n\n1. [Proton-transfer-reaction mass spectrometry for tracking trace-level volatile organic compounds](https://www.nature.com/articles/s42254-026-00990-1)\n2. [PTRMS SOP (April2025) (actris.eu)](https://actris.eu/sites/default/files/inline-files/PTRMS%20SOP%20%28April2025%29.pdf)\n3. [Advances in Proton Transfer Reaction Mass Spectrometry (PTR-MS): Applications in Exhaled Breath Analysis, Food Science, and Atmospheric Chemistry](https://pmc.ncbi.nlm.nih.gov/articles/PMC8188715/)\n4. [Identification and quantification of VOCs by proton transfer reaction time of flight mass spectrometry: an experimental workflow](https://pmc.ncbi.nlm.nih.gov/articles/PMC5838793/)\n5. [Validity and limitations of simple reaction kinetics to calculate concentrations of organic compounds from ion counts in PTR-MS (Holzinger et al., AMT 2019)](https://amt.copernicus.org/articles/12/6193/2019/amt-12-6193-2019.pdf)\n6. [PTR-MS | IONICON](https://www.ionicon.com/technologies/details/ptr-ms)\n7. [Analysis of Trace Gases at ppb Levels by Proton-Transfer-Reaction Mass Spectrometry (PTR-MS)](https://www.osti.gov/etdeweb/servlets/purl/20020157)\n8. [DOE SC ARM TR-160: Proton Transfer Time of Flight Mass Spectrometer](https://www.osti.gov/servlets/purl/1251396)\n9. [Sensitivity and specificity of atmospheric trace gas detection by proton-transfer-reaction mass spectrometry](https://www.sciencedirect.com/science/article/abs/pii/S1387380602009260)\n10. [Determination of formaldehyde mixing ratios in air with PTR-MS (Inomata et al., ACP 2008)](https://acp.copernicus.org/articles/8/273/2008/acp-8-273-2008.pdf)\n11. [Proton transfer reaction mass spectrometry: on-line trace gas analysis at the ppb level (International Journal of Mass Spectrometry and Ion Processes, 1995)](https://doi.org/10.1016/0168-1176%2895%2904294-u)\n12. [Flowing Afterglow Measurements of Ion-Neutral Reactions (Advances in atomic and molecular physics, 1969)](https://doi.org/10.1016/s0065-2199%2808%2960154-2)\n13. [The selected ion flow tube (SIFT); A technique for studying ion-neutral reactions (International Journal of Mass Spectrometry and Ion Physics, 1976)](https://doi.org/10.1016/0020-7381%2876%2980133-7)\n14. [Proton-transfer-reaction mass spectrometry (PTR–MS): on-line monitoring of volatile organic compounds at pptv levels](https://pubs.rsc.org/en/content/articlelanding/1998/cs/a827347z)\n15. [Proton-transfer-reaction mass spectrometry (PTR-MS): on-line monitoring of volatile organic compounds at volume mixing ratios of a few pptv](https://iopscience.iop.org/article/10.1088/0963-0252/8/2/314)\n16. [Robert S. Blake and colleagues (2004). Demonstration of Proton-Transfer Reaction Time-of-Flight Mass Spectrometry for Real-Time Analysis of Trace Volatile Organic Compounds. Analytical Chemistry.](https://doi.org/10.1021/ac0498260)\n17. [Martin Graus, Markus Müller, Armin Hansel (2010). High resolution PTR-TOF: Quantification and formula confirmation of VOC in real time. Journal of the American Society for Mass Spectrometry.](https://doi.org/10.1016/j.jasms.2010.02.006)\n18. [A. Jordan and colleagues (2009). An online ultra-high sensitivity Proton-transfer-reaction mass-spectrometer combined with switchable reagent ion capability (PTR+SRI−MS). International Journal of Mass Spectrometry.](https://doi.org/10.1016/j.ijms.2009.06.006)\n19. [Jordan Krechmer and colleagues (2018). Evaluation of a New Reagent-Ion Source and Focusing Ion–Molecule Reactor for Use in Proton-Transfer-Reaction Mass Spectrometry. Analytical Chemistry.](https://doi.org/10.1021/acs.analchem.8b02641)\n20. [Comparing Proton Transfer Reaction (PTR) and Adduct Ionization Mechanism (AIM) for the Study of Volatile Organic Compounds](https://www.mdpi.com/1420-3049/31/3/402)\n21. [M. Müller and colleagues (2014). A compact PTR-ToF-MS instrument for airborne measurements of volatile organic compounds at high spatiotemporal resolution. Atmospheric measurement techniques.](https://doi.org/10.5194/amt-7-3763-2014)\n22. [Isomer-Resolved Real-Time Quantification and Dynamics of Indoor Carbonyl Compounds via NO+ Chemical Ionization in PTR-MS](https://pubs.acs.org/doi/10.1021/acs.est.5c14145)\n23. [Technical Comparison - SIFT-MS and PTR-MS (Long Version)](https://gcms.cz/labrulez-bucket-strapi-h3hsga3/application::paper.paper/syft_techcom_ptrms.pdf)\n24. [Speciating volatile organic compounds in indoor air: using in situ GC to interpret real-time PTR-MS signals](https://pubs.rsc.org/en/content/articlehtml/2025/em/d4em00602j)\n25. [Product ion distributions using H3O+ PTR-ToF-MS: mechanisms, transmission effects, and instrument-to-instrument variability (AMT, 2025)](https://amt.copernicus.org/articles/18/1013/2025/)\n\n---\n*Topic: Encyclopedia › Physical world and mathematics › Chemistry › Chemical principles and methods › Analytical chemistry › Mass spectrometry methods*\n\n*Initially written Sep 29, 2026 · Reviewed: Sep 30, 2026 · Edited: Sep 30, 2026 · Last review: Sep 30, 2026*\n\n*Copyright 2026 EdgeChat AI, a subsidiary of Biostate AI.*\n\nLicense: Edgepedia Community License 1.0, https://www.edgepedia.org/edgepedia/license\n",
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 "speakable": "Proton-transfer-reaction mass spectrometry is an analytical technique that ionizes trace volatile organic compounds directly in air using hydronium ions, introduced in 1995 and used in breath analysis and atmospheric monitoring."
}