Abstract

Abstract. The ChArMEx (Chemistry and Aerosols Mediterranean Experiments) SOP2 (special observation period 2) field campaign took place from 15 July to 5 August 2013 in the western Mediterranean Basin at Ersa, a remote site in Cape Corse. During the campaign more than 80 volatile organic compounds (VOCs), including oxygenated species, were measured by different online and offline techniques. At the same time, an exhaustive description of the chemical composition of fine aerosols was performed with an aerosol chemical speciation monitor (ACSM). Low levels of anthropogenic VOCs (typically tens to hundreds of parts per trillion for individual species) and black carbon (0.1–0.9 µg m−3) were observed, while significant levels of biogenic species (peaking at the ppb level) were measured. Furthermore, secondary oxygenated VOCs (OVOCs) largely dominated the VOC speciation during the campaign, while organic matter (OM) dominated the aerosol chemical composition, representing 55 % of the total mass of non-refractory PM1 on average (average of 3.74 ± 1.80 µg m−3), followed by sulfate (27 %, 1.83 ± 1.06 µg m−3), ammonium (13 %, 0.90 ± 0.55 µg m−3) and nitrate (5 %, 0.31 ± 0.18 µg m−3). Positive matrix factorization (PMF) and concentration field (CF) analyses were performed on a database containing 42 VOCs (or grouped VOCs), including OVOCs, to identify the covariation factors of compounds that are representative of primary emissions or chemical transformation processes. A six-factor solution was found for the PMF analysis, including a primary and secondary biogenic factor correlated with temperature and exhibiting a clear diurnal profile. In addition, three anthropogenic factors characterized by compounds with various lifetimes and/or sources have been identified (long-lived, medium-lived and short-lived anthropogenic factors). The anthropogenic nature of these factors was confirmed by the CF analysis, which identified potential source areas known for intense anthropogenic emissions (north of Italy and southeast of France). Finally, a factor characterized by OVOCs of both biogenic and anthropogenic origin was found. This factor was well correlated with submicron organic aerosol (OA) measured by an aerosol chemical speciation monitor (ACSM), highlighting the close link between OVOCs and organic aerosols; the latter is mainly associated (96 %) with the secondary OA fraction. The source apportionment of OA measured by ACSM led to a three-factor solution identified as hydrogen-like OA (HOA), semi-volatile oxygenated OA (SV-OOA) and low volatility OOA (LV-OOA) for averaged mass concentrations of 0.13, 1.59 and 1.92 µg m−3, respectively. A combined analysis of gaseous PMF factors with inorganic and organic fractions of aerosols helped distinguish between anthropogenic continental and biogenic influences on the aerosol- and gas-phase compositions.

Highlights

  • Organic matter is directly emitted into the atmosphere both in the gas phase as volatile organic compounds (VOCs) and in the aerosol phase as primary organic aerosol (POA)

  • Considering the primary anthropogenic part of oxygenated VOCs (OVOCs) determined based on the anthropogenic factor contribution to OVOCs, the contribution of anthropogenic VOCs to measured VOCs rises to 42 %, which is much closer to the Positive matrix factorization (PMF) results

  • The ChArMEx SOP2 field campaign provided a unique opportunity for insight into the various sources and fates of organic carbon in the Mediterranean atmosphere, thanks to the measurement of a large panel of gaseous and aerosol species at a remote site located at Cape Corse in the western Mediterranean Basin

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Summary

Introduction

Organic matter is directly emitted into the atmosphere both in the gas phase as volatile organic compounds (VOCs) and in the aerosol phase as primary organic aerosol (POA). PMF was used at remote sites (Lanz et al, 2009; Sauvage et al, 2009; Leuchner et al, 2015), despite the need to assume mass conservation between the source location and the measurement site in this approach (Hopke, 2003) In such environments, PMF can be used as a tool to identify aged primary sources and the photochemical formation of organic trace gases. As part of the ChArMEx and CARBO-SOR projects, this study investigates the sources and the chemistry of atmospheric organic matter by combining different statistical tools, i.e., the PMF and ME-2 (multilinear engine-2) models and the concentration field method This approach was used to (i) identify the covariation factors of measured VOCs that are representative of primary emissions at various stages of aging and chemical transformation occurring during longrange transport and to (ii) better characterize the different fractions of organic aerosol. The PMF factors were used to assess the origin of non-refractive organic species in PM1 (particulate matter with an aerodynamic diameter below 1 μm) observed at the measurement site, especially to try to determine the fraction of biogenic versus anthropogenic OA

Description of the Cape Corse ground site
VOC measurements
C6–C12 n-aldehydes
Ancillary gas measurements
Aerosol measurements
PILS-IC instrument
PILS-TOC instrument
OCEC Sunset field instrument
Q-ACSM instrument
Back-trajectory classification
Photochemical age of air masses
Source-receptor models
Gas phase
Aerosol phase
Exploring the drivers of VOC variability at Cape Corse
Anthropogenic influence
Biogenic influence
Oxygenated factor
Apportionment of measured OVOC
Comparison with other PMF studies performed in remote environments
Source apportionment of OA at Cape Corse
Gas–aerosol link
Conclusions
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