Himadri Sekhar Bhowmik1, Sachchida Nand Tripathi This email address is being protected from spambots. You need JavaScript enabled to view it.2, Ravi Sahu1, Ashutosh Kumar Shukla1, Vipul Lalchandani1, Shamitaksha Talukdar1, Nidhi Tripathi3, Lokesh Sahu3 

1 Department of Civil Engineering, Indian Institute of Technology Kanpur, Kanpur, India
2 Department of Civil Engineering and Centre for Environmental Science and Engineering, Indian Institute of Technology Kanpur, Kanpur, India
3 Space and Atmospheric Sciences Division, Physical Research Laboratory, Ahmedabad, India


Received: May 3, 2022
Revised: August 9, 2022
Accepted: September 5, 2022

 Copyright The Author(s). This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are cited.


Download Citation: ||https://doi.org/10.4209/aaqr.220113  

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Cite this article:

Bhowmik, H.S., Tripathi, S.N., Sahu, R., Shukla, A.K., Lalchandani, V., Talukdar, S., Tripathi, N., Sahu, L. (2022). Insights into the Regional Transport and Local Formation of Secondary Organic Aerosol in Delhi, India. Aerosol Air Qual. Res. https://doi.org/10.4209/aaqr.220113


HIGHLIGHTS

  • Multi-day elevated SOA episodes were investigated for local or regional origin.
  • High OC/EC days were investigated for any strong primary source or SOC formation.
  • O3, CO, NO, and VOC ratios were analyzed to explore the origin of SOA.
  • However, similar sulfate dynamics with SOA consolidated the regional transport.
  • CWT plots were also used to confirm the origin and transport path.
 

ABSTRACT


The organic carbon (OC) and elemental carbon (EC) content were measured from PM2.5 quartz filter substrates collected over 24 hours in Faridabad, a heavily polluted city in Delhi national capital region (NCR), during January–February 2018. In this study, the secondary fraction of OC (SOC) was calculated using the ‘EC-tracer method’, and subsequently, secondary organic aerosol (SOA) was calculated. Some typical episodes were observed where SOA was elevated for multiple days. These occurrences were investigated for aged SOA formation through multi-day regional transport and locally generated SOA using ozone (O3), carbon monoxide (CO), nitric oxide (NO), and volatile organic compounds (VOCs) as supplementary data. Higher OC/EC ratios during these episodes could be due to a strong primary source, and this possibility cannot be ruled out. However, similar sulfate dynamics with SOA consolidated the multi-day regional transport of SOA during the elevated SOA episodes. The moderate resolution imaging spectroradiometer (MODIS) fire count and planetary boundary layer height (PBLH) data were examined to strengthen the hypothesis that the elevated SOA days were due to multi-day regional transport of SOA and not locally formed. The ratios of volatile organic compounds (VOC) were analyzed to understand the origins of VOCs and also to explore the regional transformation and local formation of SOA. The toluene/benzene (T/B) and isoprene/benzene (I/B) ratios were observed during the multi-day elevated SOA episodes to distinguish the regional and local sources of VOCs. Concentration weighted trajectory (CWT) plots also confirmed our hypothesis. This study suggests that the higher SOC fraction during those episodes was most likely due to regional or aged SOA formation. Also, multi-day regional transport contributes to the higher and elevated SOA episodes during January–February 2018.


Keywords: OC, EC, Local SOA, Regional SOA




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