Abstract

ABSTRACTSize-segregated aerosol samples (PM 7.2) were collected over Patiala (30.33°N, 76.40°E; 250 m amsl), a semi-urban city located in northwestern Indo-Gangetic Plain (IGP) during October, 2012 to September, 2013. These samples were analyzed for carbonaceous aerosols (organic carbon (OC), elemental carbon (EC) and water-soluble organic carbon (WSOC)) to study their temporal variation, prevailing emission source (s) and secondary formation processes. Annual average of total suspended particulates (TSP) concentration, estimated by adding the aerosol concentrations in different size ranges, was found to be 199 ± 82 µg m–3, varying from 88–387 µg m–3 with majority of particulate mass found in submicron size (PM 75%) and WSOC (> 80%) was observed in submicron size, suggesting that OC mainly comes from combustion and/or secondary source (s). It has been observed that almost half of OC is secondary. On the other hand, climate forcing agent EC in PM<0.95 varied from 1.1 to 9.8 µg m–3 (4.8 ± 2.2 µg m–3). High mass ratios of OC/EC (~1.5–7.2) and WSOC/OC (~0.33–0.68) indicate the relative dominance of biomass burning emission over the study region. Total carbonaceous aerosols account for ~10–59% of submicron particulates mass (PM<0.95), indicating that fine particulates are enriched with carbonaceous species. These results have implications to regional climate model development and validation.

Highlights

  • Carbonaceous aerosols consist of both light-scattering organic carbon (OC) and light-absorbing elemental carbon (EC) (Bond et al, 2004; Kondo et al, 2011)

  • It is noteworthy that the absolute mass concentration of PM

  • The present study reports year round (October, 2012– September, 2013) measurements of size-segregated particulate matter mass as well as carbonaceous aerosols (OC, water-soluble organic carbon (WSOC) and EC) concentrations over Patiala, located in the northwestern part of the Indo-Gangetic Plain (IGP)

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Summary

Introduction

Carbonaceous aerosols consist of both light-scattering organic carbon (OC) and light-absorbing elemental carbon (EC) (Bond et al, 2004; Kondo et al, 2011). This suggests that biomass burning emission is prominent source of organic aerosols as compared to vehicular emission over the study region as average mass ratio of WSOC3.0 to OC3.0 is 0.52.

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