OPEN ACCESS

Articles online

Seasonal Variations in Water Soluble Inorganic Ions, OC and EC in PM10 and PM>10 Aerosols over Delhi: Influence of Sources and Meteorological Factors

Category: Aerosol and Atmospheric Chemistry

Volume: 16 | Issue: 5 | Pages: 1165-1178
DOI: 10.4209/aaqr.2015.07.0472
PDF | Supplemental material | RIS | BibTeX

Pawan Kumar, Sudesh Yadav

  • School of Environmental Sciences, Jawaharlal Nehru University, New Delhi-110067, India

Highlights

PM10 and CA exceeded NAAQS and showed seasonal changes.
Soluble ions were more in PM10 than in CA and changes with season.
OC dominated in TC, Char dominated over soot, more SOC formation during summers.
Three sources were identified for eight fractions of TC.
WSII, OC and EC concentrations are influenced by sources and meteorological factors.


Abstract

The PM10 and particles of greater than 10 µm aerodynamic diameter (hence forth referred as PM>10) collected over Delhi exceeded the National Ambient Air Quality Standards (100 µg m–3) with an annual average of 215 µg m–3 and 495 µg m–3, respectively. The water soluble inorganic ions (WSII) were higher throughout the year in PM10 (13.5%) than in PM>10 (5%). SO42– dominated over NO3 ions and contributed 54% to the total WSII in PM10. NO3 and Ca2+ were dominant ions in PM>10. NH4+ during winter and autumn, and Ca2+ in summer PM10 samples were the major acid neutralizing species. The WSII showed monthly and seasonal changes. The total carbon (TC = EC + OC) constituted 8.8%–47.8% of total PM10 mass, and OC and EC varied from 9.91 to 37.06 µg m–3 and 5.42 to 22.23 µg m–3 during the year long sampling period. The SOC contributed more to OC in summers and the char (EC1) dominated over soot (EC2 + EC3) in EC fractions throughout the year. In summer samples, secondary OC (SOC) contributed 81% to OC and the OC/EC ratio was 3.61 suggesting the possible role of mineral dust and high photochemical activity in SOC production. For the eight different fractions, three dominant sources were identified, coal combustion, biomass burning, and motor vehicle exhaust for OC1, OC2 and OC3; vehicle exhaust for OC4, OP, EC2 and EC3; and biomass and coal combustion for EC1. The seasonal changes in the WSII and carbon concentrations in PM10 and PM>10 are attributed to both the sources and the meteorological conditions in and around the study area.

Keywords

Soluble ions Carbon fractions Processes Air quality


Related Article

PM10 Sampling and AOD Trends during 2016 Winter Fog Season in the Islamabad Region

Gufran Bulbul, Imran Shahid, Farrukh Chishtie , Muhammad Zeeshaan Shahid, Rabia Ali Hundal, Fatima Zahra, Muhammad Imran Shahzad
Accepted Manuscripts
DOI: 10.4209/aaqr.2017.01.0014
PDF

Transboundary and Local Air Pollutants in Western Japan Distinguished on the Basis of Ratios of Metallic Elements in Size-Segregated Aerosols

Yuta Taniguchi, Kojiro Shimada, Akinori Takami, Neng-Huei Lin, Chak K. Chan, Yong Pyo Kim, Shiro Hatakeyama
;