Articles | Volume 17, issue 19
https://doi.org/10.5194/amt-17-5887-2024
© Author(s) 2024. This work is distributed under the Creative Commons Attribution 4.0 License.
Evaluation of a reduced-pressure chemical ion reactor utilizing adduct ionization for the detection of gaseous organic and inorganic species
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- Final revised paper (published on 07 Oct 2024)
- Supplement to the final revised paper
- Preprint (discussion started on 19 Apr 2024)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on egusphere-2024-945', Anonymous Referee #2, 06 May 2024
- AC2: 'Reply on RC1', Matthieu Riva, 13 Jul 2024
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RC2: 'Comment on egusphere-2024-945', Anonymous Referee #1, 10 May 2024
- AC1: 'Reply on RC2', Matthieu Riva, 13 Jul 2024
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RC3: 'Comment on egusphere-2024-945', Anonymous Referee #3, 10 May 2024
- AC3: 'Reply on RC3', Matthieu Riva, 13 Jul 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 (13 Jul 2024)
Author's response
Author's tracked changes
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ED: Publish as is (18 Jul 2024) by Keding Lu
AR by Matthieu Riva on behalf of the Authors (24 Jul 2024)
This is an interesting study on a novel variation of one of the most prominent experimental techniques in atmospheric chemistry, especially aerosol-relevant chemistry. The study is written so well, that even a modeller like myself could follow the discussion, and appreciate the numerous small tweaks the authors have made to improve their setup. I can thus recommend publication essentially as is. I have some very minor comments and questions that the authors can address at their discretion, these are described below.
-line 230, “reagent ions and analyte ions that are very weakly bound to the reagent ions (e.g., water cluster with a binding energy of 42 kcal/mol)”. 42 kcal/mol is not a weak binding energy - even the most strongly bound ELVOC*NO3- clusters are typically bound by less than this. And certainly iodine-formic acids (mentioned as an example of moderate binding a few lines below) is bound by less than this. Perhaps the 42 kcal/mol value refers to the total binding energy of multiple water molecules? Or is there a unit conversion error somewhere? Please explain/elaborate.
-line 385: “(XX%)”, please update the actual number here (or explain the notation) - this looks like something that a co-author forgot to fill in during finalising of the manuscript.
-Line 448: something is grammatically wrong with the formulation of this sentence: “the formation of”… “can react”. Maybe reformulate to “The RO2 radicals generated”… “can further react”?
-Line 511: “Differences in the contribution of these compound groups with previous work could be due to different sensitivities of the instruments…”. While certainly true, isn’t it also the case that especially the formation of ELVOC and ULVOC compounds (by a combination of autoxidation and dimer formation) is very sensitive to the experimental conditions (concentrations, residence times, NOx levels, OH scavenger, temperature etc). So probably some of the differences between the present results and earlier studies are just because of subtle differences in the actual ozonolysis experiment, rather than differences between the instruments? Additionally, maybe explain a bit more in detail what specific “differences in contributions” are meant here?
-in figure S4 (in the supplementary), it is presumably values of the subscript x (indicating the number of O atoms in the three composition families) that are varied from 1 to 4. It took me a while to understand what the “O=1” etc texts in the figure meant. Please use “x=1” and so on instead, to be consistent with your own notation in the legend.