Articles | Volume 17, issue 17
https://doi.org/10.5194/amt-17-5413-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules
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- Final revised paper (published on 13 Sep 2024)
- Supplement to the final revised paper
- Preprint (discussion started on 15 Aug 2023)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on amt-2023-149', Anonymous Referee #1, 29 Sep 2023
- AC1: 'Reply on RC1', Matthieu Riva, 28 Mar 2024
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RC2: 'Comment on amt-2023-149', Anonymous Referee #2, 05 Feb 2024
- AC2: 'Reply on RC2', Matthieu Riva, 28 Mar 2024
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Matthieu Riva on behalf of the Authors (28 Mar 2024)
Author's response
Author's tracked changes
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ED: Referee Nomination & Report Request started (22 Apr 2024) by Bin Yuan
RR by Anonymous Referee #2 (09 May 2024)

ED: Publish subject to minor revisions (review by editor) (10 May 2024) by Bin Yuan

AR by Matthieu Riva on behalf of the Authors (16 May 2024)
Author's response
Author's tracked changes
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ED: Publish as is (17 May 2024) by Bin Yuan
AR by Matthieu Riva on behalf of the Authors (05 Jul 2024)
Manuscript
Review report – AMT-2023-149
The manuscript proposed by Dandan LI et al. entitled “Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules“ presents the application and potential of a new instruments for the characterisation of a large range of gas phase oxygenated organic molecules (OOMs). OOMs are essential compounds involved in SOA formation and new particle formation processes, their characterization being one of the main challenges in atmospheric chemistry. In that sense, the paper is of great interest for the international scientific community. The paper is clear, and well-structured and contains valuable information. The methodologies regarding the experiments and state of art instruments used are well described, even if some precisions could be added to some extent. The interest of the NH4+.Orbitrap is evidenced; but the results could be discussed more. As a consequence, I recommend the publication of the paper after the authors address the following points:
Main comments
2 Experimental approach and product analysis: A brief comment on how instruments other than NH4+ orbitrap have been calibrated or how quantification estimates were performed is necessary. Even if some well-established methodologies exist. This can be part of Supplementary material if the authors do not want to make the manuscript longer.
2.3 How do the authors differentiate a peak from the background? In online-MS studied; it is commonly assumed that a peak is detected when its area as 3 times higher the standard deviation of noise. Is it what has been done using ORBITOOL?
Section 3.1: I am not sure this part is necessary, because this is an illustration that an instrument with a high mass resolving power separates more easily isobaric compounds compared to instruments with a lower mass resolution. Any scientist able to understand what a mass resolution of 160 000 compared to 10 000 means is convinced that the first one is far better for separating isobaric compounds (without any demonstration needed). The interest of the paper is not the mass resolution of the orbitrap but its association to NH4+ as CI. Finally, if the authors find a justification to keep this section, I recommend them to normalize to 1 the Y scale each plot of figure 2.
Section 3.2 must be improved based on comments below:
L.287 288: Does it make sense to compare NH4+.orbitrap to another instrument (PTR-3) that is not optimised to compare OOMs? The authors showed the NH4+.orbitrap is more suited for OOMs detection, but the comparison is not on an equal foot with the PTR-3. Maybe the latter should be excluded from this study?
L.302-303: A R² > 0.5 alone is not a good criterion for “high correlation”, as it depends on the number of points associated to each sample, etc. In addition, the good correlation with other instruments could be explained by similar biases, for example. Please temper statements, or strengthen the statistical analysis.
L.353: It is not clear if the raw signal (i.e. counts) or concentrations have been used here? If raw signals are used, can the authors justify their choice? And would Figure 8 be different if the concentrations are used instead of signals?
Section 3.4: a simple comparison on couple of common compounds detected by both PTR-3 and NO3-CIMS would be nice to validate their quantification, showing there. Both instruments are used as reference to “calibrate” NH4+.orbitrap, but are PTR-3 and NO3-CIMS consistent when measuring the same compound? In addition, the NH4+.orbitrap falls in a factor 2 comparing with other instruments, which is satisfying and reasonable considering all the uncertainties associated with quantification on online-MS, but cannot be qualified as “good”, which is subjective term.
Section 3.6: the discussion is interesting here, but the results should be more detailed. For example, it is not discussed that intensity of C8 compounds increased whatever the number of O atoms, while it is more contrasted for other compounds. In addition, this increase can be up to ca. 20 for C8H12O2-4 compounds, while it is limited to 1.6 for C10, C19 and C20. Is there an explanation here? In addition, based on Figure S6, it seems the effect of RH is very important at nO<8, but what about the effect of nC? As I just mentioned, the effect of RH seemed to be stronger for C8 compounds. The increased in polarity or O/C with decreasing C number might be an explanation? This must be investigated. Figure S6 also evidenced that I-.FIGAERO-CIMS sensitivity is only decreasing with increasing RH, while it is not the case for other instruments. The authors should comment this result. Finally, as the authors cannot distinguish the effect of increasing RH on chemical and physical processes (based on experiments presented in the present paper), it is evident that RH influences NH4+.Orbitrap sensitivity, that can be different for each OOM, but this specific effect requires more attention and dedicated studies before the NH4+.Orbitrap can be used in field studies (for example, injection of pure or mixture of standards in atmospheric chamber at varying RH). From what is presented here, the understanding of RH effect on the NH4+.Orbitrap capabilities is too scarce to be able to understand the time series evolution of OOMs that would be obtained in the real atmosphere.
Minor comments:
Section 3.1: OVOCs should be replaced by OOMs, as most of detected compounds are not volatiles.
Figure 5: caption should be more explicit.
Figure 7: here the PTR-3 is probably limited compared its real potential to OOMs, because it has been tuned for efficient detection of NH4+…