Articles | Volume 19, issue 16
https://doi.org/10.5194/amt-19-5491-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Insufficient mass spectrometric detection of synthesized peroxy acids from α-pinene ozonolysis
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- Final revised paper (published on 26 Aug 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 24 Apr 2026)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on egusphere-2026-2187', Anonymous Referee #1, 16 Jun 2026
- AC1: 'Reply on RC1', Markus Tischberger, 02 Aug 2026
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RC2: 'Comment on egusphere-2026-2187', Anonymous Referee #2, 19 Jun 2026
- AC2: 'Reply on RC2', Markus Tischberger, 02 Aug 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Markus Tischberger on behalf of the Authors (04 Aug 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (06 Aug 2026) by Yoshiteru Iinuma
AR by Markus Tischberger on behalf of the Authors (06 Aug 2026)
This manuscript addresses an important issue in atmospheric measurements by examining the limitations of widely used mass spectrometric OOM measurements, particularly those arising from reagent-ion selectivity and the lack of authentic monomeric standards for hydroperoxides and peroxy acids. The topic is timely and relevant, given the central role of OOMs in secondary organic aerosol formation and new particle growth. The results suggest that peroxy acids may be systematically underestimated due to ionization-related effects, which has important implications for interpreting OOM measurements. However, several aspects of interpretation and the broader atmospheric implications require further clarification.
The central conclusion of the manuscript is that peroxy acids formed during α-pinene oxidation are substantially underdetected by nitrate-CIMS due to decomposition or fragmentation associated with the ionization process. However, the evidence presented does not fully exclude alternative explanations related to the chemical stability of the synthesized standards during storage, handling, or sampling into the instrument. Can the authors provide additional experimental evidence demonstrating that the observed discrepancy between the NMR-derived concentrations and the mass spectrometric response originates specifically from the ionization step? For example, are there measurements under different ionization conditions or inlet residence times that would help isolate the source of the signal loss? Thermal decomposition, wall losses, or inlet-related processes could contribute to the observed discrepancies. Given the known instability of peroxy compounds, can the temperature of ion transfer tube affects the stability of the cluster? Also, I suppose the total signal of the products in nitrate CIMS is the sum of normalized signal intensities of deprotonated as well as the cluster. Does addition of all the related signals (deprotonated + cluster) reduces the discrepancy observed between NMR and MS-derived ratios?
The study relies on two monomeric compounds - peroxy norpinonic acid (PNPA) and peroxy pinonic acid (PPA). This point is particularly important because the broader atmospheric implications discussed in the manuscript rely on the assumption that the behavior of the investigated standards is representative of peroxy acids present in α-pinene ozonolysis and other HOM-forming systems. This study relies on a limited number of synthesized standards, and it is unclear to what extent the results can be generalized to the broader class of highly oxygenated atmospheric peroxy acids formed during α-pinene ozonolysis.
Minor comments
1. Expansion of term HOM should be consistently defined upon first use. For example, in Line 17, HOM is expanded as ‘highly oxygenated molecules’.
2. Figure 5 middle panel figure, why the signal(m/z 247 and 231) persist in the background of the uronium ionization experiments?