Abstract

Abstract. Knowledge of the sources of carbonaceous aerosol affecting air quality in Riyadh, Saudi Arabia, is limited but needed for the development of pollution control strategies. We conducted sampling of PM2.5 from April to September 2012 at various sites in the city and used a thermo-optical semi-continuous method to quantify the organic carbon (OC) and elemental carbon (EC) concentrations. The average OC and EC concentrations were 4.7 ± 4.4 and 2.1 ± 2.5 µg m−3, respectively, during this period. Both OC and EC concentrations had strong diurnal variations, with peaks at 06:00–08:00 LT and 20:00–22:00 LT, attributed to the combined effect of increased vehicle emissions during rush hour and the shallow boundary layer in the early morning and at night. This finding suggested a significant influence of local vehicular emissions on OC and EC. The OC ∕ EC ratio in primary emissions was estimated to be 1.01, close to documented values for diesel emissions. Estimated primary organic carbon (POC) and secondary organic carbon (SOC) concentrations were comparable, with average concentrations of 2.0 ± 2.4 and 2.8 ± 3.4 µg m−3, respectively. We also collected 24 h samples of PM10 onto quartz microfiber filters and analyzed these for an array of metals by inductively coupled plasma atomic emission spectroscopy (ICP-AES). Total OC was correlated with Ca (R2 of 0.63), suggesting that OC precursors and Ca may have similar sources, and the possibility that they underwent similar atmospheric processing. In addition to a ubiquitous dust source, Ca is emitted during desalting processes in the numerous refineries in the region and from cement kilns, suggesting these sources may also contribute to observed OC concentrations in Riyadh. Concentration weighted trajectory (CWT) analysis showed that high OC and EC concentrations were associated with air masses arriving from the Persian Gulf and the region around Baghdad, locations with high densities of oil fields and refineries as well as a large Saudi Arabian cement plant. We further applied positive matrix factorization to the aligned dataset of EC, OC, and metal concentrations (Al, Ca, Cu, Fe, K, Mg, Mn, Na, Ni, Pb, and V). Three factors were derived and were proposed to be associated with oil combustion, industrial emissions (Pb based), and a combined source from oil fields, cement production, and local vehicular emissions. The dominant OC and EC source was the combined source, contributing 3.9 µg m−3 (80 %) to observed OC and 1.9 µg m−3 (92 %) to observed EC.

Highlights

  • Organic carbon (OC) and elemental carbon (EC) are key components of the atmospheric aerosol (Jacobson et al, 2000)

  • EC is emitted from a variety of combustion processes (Bond et al, 2013), classified as a short-lived climate forcer that contributes to atmospheric warming (Ramanathan and Carmichael, 2008), and associated with human morbidity and mortality (Weinhold, 2012)

  • We focus here on identifying the major sources of PM2.5 carbonaceous aerosol in Riyadh to provide a basis for formulating air pollutant mitigation strategies

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Summary

Introduction

Organic carbon (OC) and elemental carbon (EC) (or black carbon, BC, operationally identified based on detection method) are key components of the atmospheric aerosol (Jacobson et al, 2000). The contribution of carbonaceous components to total particulate matter (PM) concentrations varies with site and season, comprising from 20 to 90 % of the total mass (Kanakidou et al, 2005). OC includes both direct emissions (primary organic carbon, POC) and secondary OC (SOC) formed in the atmosphere via oxidation (Robinson et al, 2007). Mon sources of atmospheric POC and of SOC precursors are vehicular exhaust, industrial emissions, biogenic emissions, and biomass burning (Millet et al, 2005; Saarikoski et al, 2008; Genberg et al, 2011; Hu et al, 2012; Vodicka et al, 2013; Heal and Hammonds, 2014; Huang et al, 2014a, b). Except near strong emission sources, secondary organic aerosol is the main contributor to the total organic aerosol mass concentration, frequently accounting for 72 ± 21 % (Zhang et al, 2007; Jimenez et al, 2009)

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