Abstract

Abstract. We interpret here the variability of levels of carbonaceous aerosols based on a 12 yr database from 78 monitoring stations across Spain specially compiled for this article. Data did not evidence any spatial trends of carbonaceous aerosols across the country. Conversely, results show marked differences in average concentrations from the cleanest, most remote sites (around 1 μg m−3 of non-mineral carbon (nmC), mostly made of organic carbon (OC) with very little elemental carbon (EC), around 0.1 μg m−3; OC / EC = 12–15), to the highly polluted major cities (8–10 μg m−3 of nmC; 3–4 μg m−3 of EC; 4–5 μg m−3 of OC; OC / EC = 1–2). Thus, urban (and very specific industrial) pollution was found to markedly increase levels of carbonaceous aerosols in Spain, with much lower impact of biomass burning and of biogenic emissions. Correlations between yearly averaged OC / EC and EC concentrations adjust very well to a potential equation (OC = 3.37 EC0.326, R2 = 0.8). A similar equation is obtained when including average concentrations obtained at other European sites (OC = 3.60EC0.491, R2 = 0.7). A clear seasonal variability in OC and EC concentrations was detected. Both OC and EC concentrations were higher during winter at the traffic and urban sites, but OC increased during the warmer months at the rural sites. Hourly equivalent black carbon (EBC) concentrations at urban sites accurately depict road traffic contributions, varying with distance from road, traffic volume and density, mixing-layer height and wind speed. Weekday urban rush-hour EBC peaks are mimicked by concentrations of primary gaseous emissions from road traffic, whereas a single midday peak is characteristic of remote and rural sites. Decreasing annual trends for carbonaceous aerosols were observed between 1999 and 2011 at a large number of stations, probably reflecting the impact of the EURO4 and EURO5 standards in reducing the diesel PM emissions. This has resulted in some cases in an increasing trend for NO2 / (OC + EC) ratios as these standards have been much less effective for the abatement of NOx exhaust emissions in passenger diesel cars. This study concludes that EC, EBC, and especially nmC and OC + EC are very good candidates for new air quality standards since they cover both emission impact and health-related issues.

Highlights

  • Carbonaceous material typically accounts for 10 to 50 % of the total particulate matter (PM10) mass concentration (Putaud et al, 2010)

  • We focus on the following: (a) mean concentration ranges for nonmineral carbon (nmC), organic carbon (OC), EC and equivalent black carbon” (EBC); (b) inter-annual and seasonal trends; (c) OC / EC ratios; (d) EBC / EC ratios; and (e) possible origins for OC and EC

  • CLaonacraytAirocnhipoelfagtohees amndotnheitSoprainnisgh sNtoartthieornn sAfariccarnotsesrritmoriaesinfrloamnwdhSerpe ain, the dBurainlgeathreicpeariondd19C99a-n20a1r1ydaAtarocnhnimpCe,laOgCo, EeCs aannddEBtCheweSrepoabntaiinsehd.northern African territories from where data on nmC, OC, EC and EBC were obtained during the period 1999–2011

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Summary

Introduction

Carbonaceous material typically accounts for 10 to 50 % of the total particulate matter (PM10) mass concentration (Putaud et al, 2010). Particulate carbon may be classified into three components: organic carbon (OC), elemental carbon (EC, sometimes used as an equivalent to black carbon, BC) and carbonate or mineral carbon (CC). The term nonmineral carbon (nmC) is used for the concentrations of total carbon once CC has been subtracted. OC can be of both primary and secondary origin, i.e. emitted directly into the atmosphere or formed by the condensation of compounds produced in the atmosphere by photo-oxidation of volatile organic precursors (Fuzzi et al, 2006). CC is another primary carbonacous species and is present in natural dust as well as in urban dust

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