Articles | Volume 23, issue 5
https://doi.org/10.5194/acp-23-3383-2023
© Author(s) 2023. This work is distributed under the Creative Commons Attribution 4.0 License.
Real-time measurements of non-methane volatile organic compounds in the central Indo-Gangetic basin, Lucknow, India: source characterisation and their role in O3 and secondary organic aerosol formation
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- Final revised paper (published on 17 Mar 2023)
- Supplement to the final revised paper
- Preprint (discussion started on 14 Nov 2022)
- 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 egusphere-2022-1165', Anonymous Referee #1, 08 Dec 2022
- AC1: 'Reply on RC1', Sachchida Tripathi, 13 Feb 2023
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RC2: 'Comment on egusphere-2022-1165', Anonymous Referee #2, 08 Dec 2022
- AC2: 'Reply on RC2', Sachchida Tripathi, 13 Feb 2023
- AC3: 'Comment on egusphere-2022-1165', Sachchida Tripathi, 13 Feb 2023
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Sachchida Tripathi on behalf of the Authors (13 Feb 2023)
Author's response
Author's tracked changes
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ED: Publish as is (14 Feb 2023) by Ivan Kourtchev
AR by Sachchida Tripathi on behalf of the Authors (15 Feb 2023)
General Comments
This study describes the deployment of a state-of-the-art Proton Transfer Reaction Mass Spectrometer instrument for high time resolution measurements of a large range of volatile organic compounds in an urban location in India. Positive Matrix Factorization was used to apportion the sources of the measured compounds. Relationships with simultaneous measurements of PM2.5 aerosol chemical composition via High Res ToF-AMS as well as Black Carbon (BC), NOx, SO2, Ozone, meteorological parameters and back trajectory analysis were used to support the selected PMF solutions and explore temporal variations.
The ozone formation potential and SOA yield of individual VOCs as well as each identified factor were estimated. This study identified traffic, solid fuel combustion, secondary VOC formation and volatile chemical products associated with industry as the dominant sources of VOCs at the sampling site. VOCs associated with traffic and solid fuel combustion had the highest ozone formation potential and estimated SOA yield.
This work is an addition to other recent studies using HR-PTR-MS in Ahmedabad (e.g. Sahu et al 2015, 2016, 2017) and Delhi (e.g. Wang et al 2020, Tripathi et al 2022, Jain et al 2022) with associated studies using a HR-ToF-AMS (Shukla et al 2021, Lalchandani et al 2021, Tobler et al 2020) undertaken with the researchers from the Indian Institute of Technology Kanpur. While the present study is of relevance to national and regional air quality management and population health studies, the manuscript requires further work to demonstrate novelty and impact for the wider atmospheric chemistry and physics domain. In particular:
Specific Comments
Abstract
2.6 CWT back trajectory analysis
1) rename section “Concentration weighted back trajectory analysis”
2) 100m of arrival height is repeated x2 in the text.
3) Acknowledge who this method was first described by.
4) Note the reader may require explanation to reconcile why prevailing winds during study as shown in windroses in Fig S1 were predominantly from the SE – SW yet the CWT plots in fig S3 show higher trajectory density from the North.
3.1 NMVOC concentrations and temporal variation.
1) In general this section requires significant revision to clarify the aim of this section and the concepts presented to improve interpretation. Suggest here presenting
- summary stats for NMVOC, dominant species (Acetald., Acetone, Acetic Acid) and relative contributions of these species and each of the VOC families to NMVOC.
- seasonally and diurnally varying patterns
- High pollution events – provide data on NMVOC, specific air toxics eg benz, Pm2.5, ozone – which NMVOCs species/families were dominant in these episodes, what was the prevailing meterology (ie stagnant conditions in winter, high photochemistry conditions in summer?)
2) Figure 2 – include lines to indicate winter and summer periods. Note low data capture for months to Dec and to April may bias these results. In top panel ‘VOC time series’ Consider instead of plotting ‘Other” plot rel. contribution of VOC families
3) Line 264 – 266 “ the highest concentrations of NMVOCs, NR-PM2.5 during the winter months infer their common sources” – meteorology would also play an important role ie calm conditions in winter and lower PBL? Use quantitative statements ie provide NMVOC and NR-PM2.5 concs in brackets.
4) Line 266 – “In contrast, during the summer months, PM2.5 decreases drastically, but NMVOC concentrations are relatively highest, implying additional sources of NMVOCs”. – sentence requires revision.
6) Line 275 “ diurnal variations of secondary formation, anthropogenic emission level, weather and PBL heights can be explained by OVOC/ benzene ratios to some extent” revise sentence – the ratio of OVOCs/benzene does not explain these factors.
3.2 PMF results
3.2.1 Optimum solution selection
Merge this with discussion of PMF methodology in 2.4.
3.2.2 Profile and diurnal variation
1) Suggest rename / restructure this section ‘3.2 Characteristics of selected PMF factors’
4) General info on outcomes of PMF, outline info that will be presented to characterise each factor and then present detail under Sub-headings 3.2.X for each factor
2) Fig 5 – add formula/name to key peaks. Figures 6 and 7 are useful as is. Fig 8 – check AMS species labels are the same as presented in text (ie MO-OOA and LO-OOA). Figure 9c while r2 value is 0.52 the plot indicates a poor relationship.
3) Add time series of factors – consider adding to Fig 2 to aid comparison with other variables.
5) Use consistent presentation of characteristics for each factor
- Factor identification ie traffic, SFC1, SFC 2
- Marker species and their average % contribution to the factor.
- relationships to other atmospheric species – move discussion from 3.3 under each relevant sub-heading
- diurnal / seasonal patterns which help identify sources eg diurnal patterns that align with peak traffic; seasonal patterns of SFC.
- CWT plots for each factor – do they align with location of known / likely sources?
- comparison with previous studies – similar markers and % contributions?
3.4 OFP and SOA yield from individual sources
1) Is there a relationship between factors/ species with high SOA and O3 potential and measured concentrations of SOA and O3? Consider a time lag in peaks.
2) This section would be improved by comparison with previous studies and discussion on relevance of this section ie for control strategies to reduce O3 and SOA.
3) The limitations of these approaches should be noted – these are estimates of potential for ozone and SOA formation not actual yields of ozone and SOA.
1) This section should be used to synthesise what has been learnt from this and the previous studies – what factors are common to Indian/Asian cities and which are different- consider a mapped pie chart type plot for NMVOCs and NR-Pm2.5 composition like that shown in Zhang 2007.
2) Line 546 “ The NMVOCs and NOx derive from the formation of ozone and SOA, but there is limited knowledge of their complex relationship” – sentence needs revising. Reverse relationship is true – The formation of ozone and SOA is driven by the oxidation of NMVOCs. The purpose of this statement is not clear.
3) The overall significance of this work in understanding and better managing air quality in Lucknow and other Indian cities needs to be stated.