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Article

Temporal Distribution and Gas/Particle Partitioning of Polycyclic Aromatic Hydrocarbons (PAHs) in the Atmosphere of Strasbourg, France

by
Supansa Chimjarn
1,
Olivier Delhomme
1,2 and
Maurice Millet
1,*
1
Centre National de la Recherche Scientifique, Institut de Chimie et Procédés pour l’Energie et la Santé, Université de Strasbourg, (ICPEES UMR 7515), F-67000 Strasbourg, France
2
Department of Science and Technology, Université de Lorraine, F-57070 Metz, France
*
Author to whom correspondence should be addressed.
Atmosphere 2021, 12(3), 337; https://doi.org/10.3390/atmos12030337
Submission received: 10 February 2021 / Revised: 26 February 2021 / Accepted: 2 March 2021 / Published: 5 March 2021
(This article belongs to the Special Issue Air Pollution and Environment in France)
Browse Figures
Versions Notes

Abstract

:
Gas and particulate phase ambient air concentrations of polycyclic aromatic hydrocarbons (Ʃ16PAHs) were determined in Strasbourg, a large city located in the Alsace region of northeastern France, from May 2018 to March 2020, to study the evolution of their temporal variations and their potential origins. The analysis of PAHs was performed using a global analytical method permitting the quantification of pesticides, PAHs, and polychlorobiphenyls (PCBs). Filters and Carbon doped silicon carbide NMC@SiC foams were extracted by accelerated solvent extraction (ASE) followed by a solid-phase extraction (SPE). Afterwards, extracts were analyzed using gas chromatography coupled to tandem mass spectrometry (GC-MS/MS). Prior to analysis, a pre-concentration step based on solid-phase microextraction (SPME) was used with a polydimethylsiloxane (PDMS) 100 µm fiber. The average total (gas plus particulate) concentration of Ʃ16PAHs varied from 0.51 to 117.31 ng m−3 with a mean of 16.87 ng m−3, with higher concentrations in the cold season of more than 2.5-fold and 6-fold that in the warm season for the gas and particulate phases, respectively. Moreover, low molecular weight (LMW) (2-ring and 3-ring) and medium molecular weight (MMW) (4-ring) PAHs contribute dominantly to the gas phase, while the particulate phase is associated with MMW (4-ring) and high molecular weight (HMW) (5-ring and 6-ring) PAHs. Gas/particle partitioning coefficient (log Kp) was calculated, and values varied between −4.13 and −1.49. It can be seen that the log Kp increased with the molecular weight of the PAHs and that the log Kp is different between cold and warm seasons for HMW PAHs but not for LMW PAHs. Diagnostic ratios of PAHs, which were employed to estimate the primary source of PAHs in Strasbourg, indicate that fuel combustion and biomass/coal burning are the possible origins of PAHs in Strasbourg’s atmosphere.

1. Introduction

Among the large number of atmospheric pollutants, polycyclic aromatic hydrocarbons (PAHs) are of great importance as these compounds, composed of two or more aromatic rings, are recognized as carcinogenic and mutagenic and consequently classified as priority pollutants by the American Environmental Protection Agency ‘US EPA), the European Union, and the International Agency for Research on Cancer (IARC).
PAHs are ubiquitous contaminants and are derived mostly from anthropogenic origins of incomplete combustion, such as petrol and diesel engines, automobile exhaust, domestic heating, biomass burning, and various industrial activities. They can also originate from natural sources such as forest fires and volcanic eruptions [1]. Due to their relatively low vapor pressure, they can remain in the atmosphere for a long time and be transported over long distances [2,3]. Therefore, PAHs are considered long-range transport pollutants [4] and are found in all environmental compartments such as water, soils, vegetation, and dust [5,6]. In addition to their remanence in the environment, PAHs are important for their adverse toxicological [7,8,9,10] and ecotoxicological properties [11,12].
As PAHs are ubiquitous, toxic contaminants, they have been intensively monitored in the atmosphere [13,14,15,16,17,18,19]. One important source of PAH pollution in the urban atmosphere is caused by diesel and gasoline traffic emissions [20,21]. In large cities, traffic is generally heavy and congested and can generate significant emissions of PAHs. Some variations in emissions can occur according to the period of time, in particular when emissions from domestic heating are added to vehicle emissions in winter for example [13]. The importance of the different sources of PAHs in the urban atmosphere can be tentatively estimated by the calculation of the specific ratio of some particular PAHs [22]. It is thus valuable to determine the atmospheric levels and origins of PAHs in the urban atmosphere, since the risk of human exposure could be significant for the inhabitants.
This study presents the continuous monitoring (on a weekly basis) of PAHs in the background atmosphere of Strasbourg, a very polluted large city situated in the east of France, between May 2018 and March 2020, for the evaluation of the temporal variations of concentrations and their potential origins.

2. Materials and Methods

2.1. Reagents and Chemicals

Acetonitrile (ACN), ethyl acetate (EtAc), nitric acid, ethanol (EtOH), n-hexane (n-hex), methylene chloride (DCM), and toluene (TOL) of HPLC grade were purchased from VWR, France. Polydimethylsiloxane (PDMS) 100 µm solid-phase microextraction (SPME) fibers and N-tert-butyldimethylsilyl-N-methyltrifluoroacetamide (MtBSTFA) were purchased from Sigma-Aldrich (St. Quentin Fallavier, France). Ultrapure water was obtained using an Elga system (VEOLIA, Antony, France). CHROMABOND® HLB solid-phase extraction (SPE) cartridges were purchased from Macherey-Nägel (Hoerth, France).
Mixtures of PAHs at 0.1 g L−1 in ACN were obtained from Cluzeau Info Labo (St Foy la Grande, France). Information on the PAHs used are shown in Supplementary Materials Table S1. A working mixture at 10 mg L−1 was prepared in ACN. These solutions were stored at −18 °C. Naphtalene-d8, phenanthrene-d10, chrysene-d12, and perylene-d12 at 0.01 g L−1 in ACN were used as internal standards (IS) and were obtained from Sigma-Aldrich (St. Quentin Fallavier, France).

2.2. Sampling Site and Collection

Samples were collected using a low-volume sampler (2.3 m3 h−1, Sven Leckel, Berlin, Germany) equipped with a PM10 head on a 47 mm glass fiber filter (WhatmanTM), followed by a silicon carbide foam coated with a thin layer of nitrogen-doped carbon (NMC@SiC). These foams were obtained from SICAT France [23].
Sampling was performed on a weekly basis between 15 May 2018 and 03 March 2020 in Strasbourg, a large city located in the Alsace region of northeastern France with the Vosges Mountains to the west and the Black Forest to the east. Strasbourg is an urban city containing shops, restaurants, residential areas, and the University of Strasbourg. Sampling was conducted on the roof of the University’s Botanic Institute (48.58.40°, 7.76.63°, 30 m a.g.l.), which was situated approximately 3 km from major highways and industrial areas, 11 km from the regional airport, and 3.5 km from agricultural areas. The sampling site can be considered a typical background urbanized site. During the entire sampling period, it was not always possible to effect the weekly sample for organizational and maintenance reasons. The longest periods without realizing sampling were from 17 July 2018 to 4 September 2018, from 11 December 2018 to 19 February 2019, and from 23 July 2019 to 27 August 2019.
Prior to the sampling, filters and foams were subjected to cleaning by accelerated solvent extraction (ASE) using a mixture of n-hex/DCM (50:50, v/v) followed by ACN at 1500 psi for 45 min. The ASE procedure applied consisted of three static cycles at 150 °C for 15 min each. Afterwards, samplers were wrapped in aluminum foil and stored at 50 °C.

2.3. Extraction Sample Preparation of Filters and Foams

The analysis of PAHs was performed using a global analytical method permitting the quantification of pesticides, PAHs, and polychlorobiphenyls (PCBs) [24]. In the following, the entire method procedure is described but only data for PAH quantification are detailed.
Filters and NMC@SiC foams were extracted by ASE twice using ACN at 1500 psi for 10 min at 150 °C. After extraction, MtBSTFA was added onto the ASE extract (80 mL) in order to derivatize some polar compounds (pesticides, phenols, and acids) for 1 h at 80 °C. After derivatization, these extracts (80 mL) were then diluted to 1000 mL with distilled water acidified by nitric acid (pH = 3), followed by cleaning on CHROMABOND® HLB SPE cartridges using a DIONEX® AutoTrace 280 SPE system (Lévy et al. 2020).
The SPE procedure used was as follows: first the HLB adsorbents were conditioned with respectively 5 mL of EtOH and water, and then the ASE extracts (1000 mL) were loaded at 5 mL min−1 into the SPE cartridges. Afterwards, cartridges were dried under a nitrogen steam for 30 min, and finally the analytes were consecutively eluted using 2 mL of each of the following solvents: DCM, EtAc, and ACN at 5 mL min−1.
The collected extracts were gently concentrated to a droplet under a fume hood and finally dissolved in 1 mL of ACN. Then, 100 µL of the reconstituted extract was transferred into a vial for LC-MS/MS analysis, and 10 µL of a 1 mg L−1 internal standard solution was added. The remaining 900 µL was divided into four fractions of 225 μL. One of them was re-diluted to 20 mL using acidified and salted (pH 3; 1.5% NaCl) distilled water, and 10 µL of the appropriate IS 10 mg L−1 was added for GC-MS/MS analysis in order to promote their chromatographic analysis for pesticides including organochlorine pesticides (OCPs), PAHs, and polychlorobiphenyls (PCBs) as described in the method developed by Lévy et al. (2020).

2.4. Analysis of PAHs in Sample Extracts

The analysis of PAHs was performed on a TRACETM GC equipped with a split/splitless injector (splitless for 3 min) and an Optima® XLB capillary column (30 m × 0.25 mm, 0.25 µm), coupled to an ITQTM 700 ion trap mass spectrometer. Ionization was done in internal standard mode (EI mode). Details of the MRM method for PAHs are summarized in Supplementary Material Table S1. The injector, ion source, and transfer line were heated at 250 °C, 210 °C, and 300 °C, respectively. The oven ramp was as follows: 50 °C for 3 min; followed by an increase in the temperature to 255 °C at 10 °C min−1 to finally increase to 330 °C at 20 °C min−1 where it was maintained for 18 min. Helium with high purity (≥99.999%) was used as the carrier gas at 1 mL min−1.

2.5. SPME for GC-MS/MS Analysis

Prior to GC-MS/MS analysis, the obtained 20 mL acidified extracts were re-concentrated by SPME using a CTC CombiPAL autosampler. PAHs were extracted at 80 °C for 40 min using a polydimethylsiloxane (PDMS) 100 µm fiber.

2.6. QA/QC

Two blank series were prepared; the first consisted of pre-cleaned samplers extracted and analyzed, while the second consisted of a field blank sampler extracted and analyzed. These later were packed pre-cleaned after field exposition for the same duration as field samplers. None of the assessed molecules were detected in the analyzed blank samplers, which confirms the efficiency of the cleaning and storage procedures used.
SPE was done in triplicate for each of the assessed compounds in order to calculate an average recovery rate (%).
Matrix matched calibration curves were dressed by spiking NMC@SiC foam with 1, 10, 25, 50, 100, 250, 500, and 1000 ng of pollutants. All curves were dressed in triplicate. These calibration curves were used for PAH quantification in filters as it was not possible to spike filters with standardized particles containing PAHs.
Repeatability was tested by spiking on the same day, using 5 NMC@SiC foams with 3 levels of concentration 10, 100, and 1000 ng of pollutants. In fact, spiked foams were extracted and prepared at the same time and analyzed on the same day. This experiment was repeated for three successive weeks. It should be noted that the intra-day precision (repeatability) of the assay was estimated by calculating the relative standard deviation (RSD) for the analysis of QC samples in 3 replicates, while the inter-day precision (reproducibility) was determined by the analysis of the replicate QC samples on three consecutive weeks. All extraction and concentration steps were done in triplicate, and recoveries were between 65% and 98% for the assessed congeners, which agrees with the US EPA 1668a norm.
Limits of detection (LOD) and quantification (LOQ) were calculated based on a signal to noise ratio of 3:1 and 10:1 basis, respectively, following these equations:
−LOD = 3 × [Cmin]/(S/N)
LOQ = 10 × [Cmin]/(S/N)
where [Cmin] = minimal concentration, S = signal detected at this concentration, and N = noise. Moreover, uncertainties on each congener were calculated and shown to be in the range of 3–20%. Limits of detection and quantification are summarized in Supplementary Material Table S1.

2.7. G/P Partitioning

Gas-particle distribution coefficient Kp (m3 µg−1) was calculated for PAHs using the following formula (Equation (1)) proposed by Yamasaki et al. (1982) [25]:
Kp = (Cp/TSP)/Cg
where TSP is the concentration of total suspended particulate matter (µg m−3), and Cp and Cg are the compound concentrations in the particulate and in the gas phase, respectively. TSP values were obtained from the Atmospheric Pollution Survey network (“Atmo Grand-Est”).

3. Results

3.1. Annual Concentration and Seasonal Variability of PAHs

PAHs were determined from May 2018 to March 2020 in the air of the Strasbourg area. The mean concentration of each PAH is presented in Table 1. The average total concentration of Ʃ16PAHs in the air (gas and particulate phases) was 16.87 ng m−3 (min: 0.51 ng m−3 and max: 117.31 ng m−3).
The mean concentration obtained was comparable to that measured in the urban area of Marseille (21.79 ng m−3), the largest city in the South of France [26], and in the urban area of Grenoble (Ʃ16PAHs 23.11 ng m−3), France [27]. However, this mean PAH concentration was not in the same degree as the study by Morville et al. (2011) [13] relative to atmospheric gas and particulate phases collected from 2002 to 2004 at the same site in Strasbourg. These authors found a mean concentration of Ʃ17PAHs of 149 ng m−3, which is more than 8 times higher than the concentration found in this study (16.87 ng m−3). This very different value is caused by the higher concentrations of low molecular weight PAHs (MW < 202) as NAP (43.9 > 4.27 ng m−3), PHE (24.5 > 1.72 ng m−3), ACE (20.3 > 0.66 ng m−3), FLU (9.7 > 0.52 ng m−3), FLA (9.1 >1.24 ng m−3), ANT (2.3 > 0.40 ng m−3), and PYR (4.8 > 0.40 ng m−3), while the concentrations of HMW PAHs obtained by the two studies were not significantly different. The difference in the profile of LMW PAH distribution at the Strasbourg site between the two studies can probably be explained by the different types of active samplers used, with different duration and time. More precisely, in the previous report by Morville et al. (2011), a high-volume sampler performed for 4 h with three time intervals per day (time interval of high vehicle traffic) for a few days a month in each season was used, while this study used a low-volume sampler performed on a weekly basis throughout the year. The age of the data in the previous study (from 2002 to 2004) and the period to which they relate are also important factors to explain the difference with our recent work.
The annual trends of Ʃ16PAH concentrations in both gas and particulate phases with temperature are presented in Figure 1.
For gas phase samples, the mean concentration of Ʃ16PAHs was 11.36 ng m−3, with a maximum of 79 ng m−3 on 12 to 19 November 2019, with a temperature of 4.8 ± 0.91 °C, and a minimum of 0.74 ng m−3 on 29 May to 5 June 2018, with a temperature of 22.4 ± 1.46 °C. The PAH concentration in the particulate phase was considerably lower, with a mean value of 5.51 ng m−3, and ranged from 0.29 to 21.73 ng m−3.
Additionally, the average concentrations of Ʃ16PAHs in gas and particulate phases during each season in 2018 and 2019 with the temperature and concentration of total suspended particles (TSP) are presented in Figure 2.
The seasonal variability of PAHs shows higher concentrations in autumn and winter and lower concentrations in spring and summer. For the gas phase, the maximum concentration was observed in spring, and it decreased slightly in winter with lower temperature, while the minimum concentration was in spring, and it got slightly higher in summer with higher temperature (warm and non-heating season). Moreover, a strong variation can be observed between 2018 and 2019 in the gas phase; this observation can be probably explained by lower temperature in 2019 than 2018, except in the summer period (average temperature of 21.2 °C in 2018 and 20.8 °C in 2019). Indeed, the average temperature values are 20.2 °C in 2018 and 14.4 °C in 2019 during the spring period, 10.1 °C in 2018 and 7.1 °C in 2019 during the autumn period, and 9.2 °C in 2018 and 6.5 °C in 2019 during the winter period (Figure 2). For the particulate phase, the PAH concentrations have a similar trend to the study by Delhomme et al. (2012) [14], which reported PAH concentrations in PM10 during each season.
The Ʃ16PAH concentrations in the particulate phase have a minimum in summer and increase from spring to winter, and in 2018 and 2019, a small variation between both years was found. The light difference in concentrations for the particulate phase in both years is probably due to the slightly different concentrations of TSP in the air. From the literature, the temperature and meteorological conditions are important factors influencing the distribution of PAHs for seasonal behavior of PAHs in the atmosphere [28,29]. A lower PAH concentration in the warm season and a higher concentration in the cold season were reported in numerous studies [30,31,32]. Besides the meteorological factors, the emission source of PAHs is the main factor for seasonal variations [33]. In this study, the PAH concentration in the cold season was approximately 2.5-fold and 6-fold more than that in the warm season for the gas and particulate phases, respectively.

3.2. Gas-Particle Partitioning

The profiles of relative distribution of PAHs by number of rings for four seasons in Strasbourg were studied (Figure 3).
In this study, low molecular weight (LMW) (2-ring and 3-ring) and MMW (4-ring) PAHs contribute dominantly to the gas phase, while the particulate phase is associated with MMW (4-ring) and HMW (5-ring and 6-ring) PAHs. This result shows the same trend as a number of previous studies [34,35]. The concentration of low-ring PAHs (99% of 2-ring and 95% of 3-ring) was found to be higher in the gas phase than in the particulate phase due to their high vapor pressures and low octanol-air partition coefficient. For the 4-ring PAHs, they were found in similar composition in both phases with a little bit more in the gas phase (64%), while 80% of HMW (5-ring and 6-ring) PAHs were measured in the particulate phase. Furthermore, the concentration of 2-ring PAHS in the gas phase increased with the decreasing of the temperature. This observation is probably due to the low level of photochemical reactions on 2-ring PAHs with lower temperature. For the concentration of 3-ring and 4-ring PAHs, the gas phase was slightly higher in summer than winter. This trend was the same as that reported by Li et al. (2006) [29], implying that under higher ambient temperature, 3-ring and 4-ring PAHs contaminated at ground surface were evaporated [36,37]. In the particulate phase, the dominance of 4-ring, 5-ring, and 6-ring PAHs was higher in the cold season than in the warm season. The increase in these compounds was influenced by the emission source such as combustion of vehicle automobiles and combustion of domestic heating.
Figure 4a,b presents the mean concentrations in the gas and particulate phases for each season for each PAH and illustrates the partitioning described before. It can be noted that the PAHs quantified in autumn present the highest concentrations in many cases, and this observation could be explained by the meteorological conditions which are in favor of a stagnation of pollutants in the Rhine Valley in this season.
The log Kp for each PAH was calculated from Equation (1) for the warm and cold periods (Figure 5). It can be seen that the log Kp increased with the molecular weight of the PAH. This result indicates that the proportion of the PAHs in the particulate phase related to the total concentration is more important in high molecular weight PAHs in comparison to low molecular weight PAHs. The values of log Kp varied between −4.13 and −1.49 and are consistent with previous data [19,38,39]. It can also be observed that the log Kp is different between cold and warm seasons for high molecular weight PAHs but not for low molecular weight PAH. This observation confirms the influence of meteorological conditions on the partitioning of PAHs in the atmosphere.

3.3. Diagnostic Ratios for Source Identification of PAHs

The PAH profiles in the atmosphere can be influenced by atmospheric conditions (temperature, solar radiation, wind) and by the sources of PAHs, which can be identified by the concentration of some marker compounds and their diagnostic ratio [40]. The common analytical tool to distinguish petrogenic and pyrogenic sources is to study simultaneously the ratio of the isomers of molecular weight 178 (ANT and PHE) [41]. Low values (<0.1) for this ratio are usually attributed to petrogenic sources, while a ratio greater than 0.1 indicates pyrogenic sources [42], and more precisely, points out that combustion is an important source of PAHs [43,44]. In this study, the range values of ANT/(ANT + PHE) ratio varied between 0.08 and 0.26, with an average of 0.17 ± 0.05, suggesting that a mix of petroleum and combustion sources could be the possible source of atmospheric PAHs in the Strasbourg area.
Some studies also used the ratio between the isomers with molecular weight 202 (FLA and PYR) and 276 (IcdP and BghiP) to discriminate petrogenic sources, petroleum combustion, biomass, and coal combustion [45,46]. If the values of FLA/(FLA + PYR) and IcdP/(IcdP + BghiP) are below <0.4 and <0.2 respectively, this implies a petrogenic source, while a ratio between 0.4–0.5 and 0.2–0.5 suggests that the possible source is fossil fuel combustion. A ratio greater than 0.5 is characteristic of wood, grass, or coal combustion [16]. Figure 6 shows the distribution ratios of FLA/(FLA + PYR) versus IcdP/(IcdP + BghiP) for the warm period (squares indicate temperature range 13–24 °C) and cold period (dots indicate temperature range 1–12 °C), obviously possibly pointing out the different major emission origins of PAHs. The ratio of FLA/(FLA + PYR) ranged from 0.40 to 0.87 with an average of 0.61 ± 0.19 for the warm period, and from 0.36 to 0.91 with an average of 0.67 ± 0.17 for the cold period. The IcdP/(IcdP + BghiP) was between 0.34 and 0.54 with an average of 0.42 ± 0.08 for the warm period, and between 0.23 and 0.62 with an average of 0.45 ± 0.11 for the cold period. All of these two ratios indicate that fuel combustion and biomass/coal burning are the possible origins of PAHs in Strasbourg. In France, the main source of PAHs (>55%) is the residential/tertiary sector and in Alsace, with more than 87%, emissions are due to domestic heating with wood and due to the transport sector by diesel and gasoline combustion [47,48]. These data confirmed the results obtained in this work, in which the concentrations of atmospheric PAHs in Strasbourg are mainly the consequence of emissions from combustion of wood, diesel, and gasoline. The distribution of IcdP(IcdP + BghiP) ratios for the warm period (squares) is more present in the fuel combustion zone than in the biomass zone, while the ratio for the cold period is similarly distributed in both zones. This observation is probably due to the increase in wood burning for heating in the cold period.
Additionally, Table 2 lists the diagnostic ratios of some PAHs such as PHE/(PHE + ANT), FLA(FLA + PYR), BaP/(BaP + CHR), IcdP/(IcdP + BghiP), and BaP/(BaP + BeP), which have been usually used as indicators to distinguish their origins [37,49,50].
In 2018, the ratios of PHE/(PHE + ANT) were 0.77 ± 0.13, 0.69 ± 0.21, 0.87 ± 0.12, and 0.80 ± 0.12 for spring, summer, autumn, and winter, respectively, and these ratios were similar to the literature and have been reported from emissions by gasoline vehicles (0.77 ± 0.10), diesel vehicles (0.73 ± 0.18), and wood combustion (0.84 ± 0.16). The ratio of BaA/(BaA + Chry) is generally used to evaluate the contribution of vehicular emissions.
The values obtained in this study were 0.42 and 0.47 in spring, 0.36 and 0.39 in summer, 0.40 and 0.42 in autumn, and 0.42 and 0.51 in winter. The reported literature values for this ratio were 0.22–0.55, 0.38–0.64, and 0.42, for gasoline, diesel, and wood respectively. This information confirms the importance of gasoline, diesel, and wood combustion in Strasbourg’s atmosphere.
In the summer season, the ratios of FLA/(FLA + PYR) (0.42–0.45), BaP/(BaP + CHR) (0.36–0.39), and IcdP/(IcdP + BghiP) (0.24 and 0.38) were lower than those observed in winter. The lower summer values of the ratios are explained by the decreasing of wood combustion in the summer. All the ratios considered have shown that the emission sources of PAHs in the Strasbourg area are not well defined, but there is evidence that emission of PAHs from diesel, gasoline, and wood combustion occurred at the same time.

4. Conclusions

In this study, the temporal characteristics of PAHs in the gaseous and particulate phases were studied from May 2018 to March 2020 at an urban site in Strasbourg, in the northeastern region of France. This study provides data on the PAH concentrations and variabilities for a typical large metropolis, with important activities around it, situated in a Rhine Valley. The annual trends of Ʃ16PAH concentration in both gas and particulate phases with temperature were studied, and it was found for gas phase samples that the mean concentration of Ʃ16PAHs was 11.36 ng m−3, with a maximum of 79 ng m−3 on 12 to 19 November 2019, with temperature 4.8 ± 0.91 °C, and a minimum of 0.74 ng m−3 on 29 May to 5 June 2018, with temperature 22.4 ± 1.46 °C. The PAH concentration in the particulate phase was considerably lower, with a mean value of 5.51 ng m−3, and ranged from 0.29 to 21.73 ng m−3. The seasonal variability of PAH concentrations was observed in accordance with known behavior, with higher values in autumn and winter and lower values in spring and summer. For the gas phase, the maximum concentration was in spring, with a slight decrease in winter with lower temperature, and the minimum concentration was in spring, with slightly higher concentrations in summer with a higher temperature (warm and non-heating season). Moreover, the profiles of relative distribution of PAHs with different numbers of rings for four seasons in Strasbourg were studied, and the results indicate that LMW (2-ring and 3-ring) and MMW (4-ring) PAHs contribute dominantly to the gas phase, while the particulate phase is associated with MMW (4-ring) and HMW (5-ring and 6-ring) PAHs. The values of log Kp confirm the influence of meteorological conditions on the partitioning of PAHs in the atmosphere. Finally, a trend may be established using the diagnostics ratios, with fuel combustion and biomass/coal burning being the possible origins of PAHs in Strasbourg. These origins are not defined, but there is evidence that emissions of PAHs from diesel, gasoline, and wood combustion occurred at the same time.

Supplementary Materials

The following are available online at https://www.mdpi.com/2073-4433/12/3/337/s1, Table S1: MS parameters, LOD, and LOQ for the 16 analyzed PAHs.

Author Contributions

Conceptualization, S.C., O.D. and M.M.; methodology, S.C. and M.M.; validation, S.C.; formal analysis, S.C. and O.D.; writing—original draft preparation, S.C. and O.D.; writing—review and editing. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Conflicts of Interest

The authors declare no conflict of interest.

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Atmosphere 12 00337 g001 550
Figure 1. Annual variations of gas and particulate phase PAH concentrations and temperatures from 15 May 2018 to 17 March 2020.
Figure 1. Annual variations of gas and particulate phase PAH concentrations and temperatures from 15 May 2018 to 17 March 2020.
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Atmosphere 12 00337 g002 550
Figure 2. Average concentrations of Ʃ16PAHs in the particulate and gas phases for four seasons with temperature and total suspended particles (TSP).
Figure 2. Average concentrations of Ʃ16PAHs in the particulate and gas phases for four seasons with temperature and total suspended particles (TSP).
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Atmosphere 12 00337 g003 550
Figure 3. Concentration of PAHs with different numbers of rings in the particle and gas phases for four seasons.
Figure 3. Concentration of PAHs with different numbers of rings in the particle and gas phases for four seasons.
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Atmosphere 12 00337 g004 550
Figure 4. Mean concentration in the gas (a) and particulate phase (b) for each PAH for each season. Error bars represent the standard deviation of the mean compound concentration for all samples in each season.
Figure 4. Mean concentration in the gas (a) and particulate phase (b) for each PAH for each season. Error bars represent the standard deviation of the mean compound concentration for all samples in each season.
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Atmosphere 12 00337 g005 550
Figure 5. Comparison of the warm and cold seasons with the log Kp of the 16 PAHs. Error bars represent the standard deviation of the mean compound value for all samples in each period.
Figure 5. Comparison of the warm and cold seasons with the log Kp of the 16 PAHs. Error bars represent the standard deviation of the mean compound value for all samples in each period.
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Atmosphere 12 00337 g006 550
Figure 6. Ratio of FLA/(FLA + PYR) versus IcdP/(IcdP + BhiP) for the warm (16 May–23 October 2018 and 16 April–29 October 2019) and cold (23 October 2018–16 April 2019 and 6 November 2019–17 March 2020) time periods.
Figure 6. Ratio of FLA/(FLA + PYR) versus IcdP/(IcdP + BhiP) for the warm (16 May–23 October 2018 and 16 April–29 October 2019) and cold (23 October 2018–16 April 2019 and 6 November 2019–17 March 2020) time periods.
Atmosphere 12 00337 g006
Table
Table 1. Annual mean concentrations of individual polycyclic aromatic hydrocarbons (PAHs) quantified in gas and particulate phases.
Table 1. Annual mean concentrations of individual polycyclic aromatic hydrocarbons (PAHs) quantified in gas and particulate phases.
n (%)Annual Average Concentration (min–max)
GasParticleGas (ng m−3)Particle (ng m−3)ƩG + P (ng m−3)
Naphtalene (NAP)96484.20 (0.005–25.87)0.05 (0.001–0.78)4.25 (0.005–25.90)
Acenaphtene (ACE)97570.63 (0.030–2.56)0.03 (0.001–1.89)0.66 (0.03–2.56)
Fluorene (FLU)98840.51 (0.003–2.33)0.01 (0.001–0.08)0.52 (0.04–2.33)
Phenanthrene (PHE)1001001.66 (0.003–19.05)0.06 (0.005–0.23)1.72 (0.005–19.20)
Anthracene (ACE)74480.33 (0.003–6.20)0.07 (0.001–0.91)0.40 (0.003–6.20)
Fluoranthrene (FLA)97910.82 (0.002–11.55)0.42 (0.024–1.83)1.24 (0.002–11.98)
Pyrene (PYR)97930.66 (0.004–13.28)0.23 (0.005–2.06)0.89 (0.05–13.65)
Benz(a)anthracene (BaA)971000.77 (0.004–7.53)0.65 (0.014–2.44)1.42 (0.035–8.79)
Chrysene (CHR)971000.33 (0.002–3.21)0.28 (0.006–1.04)0.61 (0.015–3.54)
Benzo(b)/(k)fluoranthrene (BaF/BkF)81970.27 (0.004–2.87)0.30 (0.022–1.81)0.57 (0.004–3.44)
Benzo(e)pyrene (BeP)86980.23 (0.002–2.94)0.21 (0.008–1.57)0.44 (0.008–3.46)
Benzo(a)pyrene (BaP)881000.14 (0.002–1.68)0.35 (0.004–3.99)0.49 (0.006–5.53)
Dibenz(a.h)anthracene (DBahA)38670.25 (0.02–0.57)0.66 (0.08–2.16)0.91 (0.08–2.20)
Indenol(1,2,3)pyrene (IndP)33400.29 (0.03–0.87)1.04 (0.125–3.73)1.33 (0.13–3.73)
Benzo(g,h,i)perylene (BghiP)45720.27 (0.057–0.84)1.15 (0.094–4.38)1.42 (0.094–5.19)
Ʃ16PAH11.36 (0.174–101.35)5.51 (0.391–28.90)16.87 (0.51–117.70)
n: percentage of positive samples detected in the gas and particulate phases.
Table
Table 2. Comparison among PAH ratios obtained from samples from this study for four seasons and possible emission sources in the Strasbourg area.
Table 2. Comparison among PAH ratios obtained from samples from this study for four seasons and possible emission sources in the Strasbourg area.
SeasonsDiagnostic Ratio
PHE/(ANT + PHE)FLA/(FLA + PYR)BaP/(BaP + CHR)IcdP/(IcdP + BghiP)BeP/(BaP + BeP)
This studySP20180.77 ± 0.130..69 ± 0.200.47 ± 0.140.41 ± 0.020.44 ± 0.24
SP20190.78 ± 0.210.68 ± 0.160.42 ± 0.070.47 ± 0.060.30 ± 0.07
S20180.69 ± 0.210.42 ± 0.130.36 ± 0.170.38 ± 0.110.44 ± 0.30
S20190.87 ± 0.020.45 ± 0.200.39 ± 0.180.24 ± 0.150.55 ± 0.08
A20180.87 ± 0.120.67 ± 0.230.40 ± 0.150.32 ± 0.100.53 ± 0.16
A20190.84 ± 0.110.61 ± 0.170.42 ± 0.160.47 ± 0.040.47 ± 0.11
W20180.80 ± 0.120.82 ± 0.130.48 ± 0.140.51 ± 0.090.33 ± 0.11
W20190.92 ± 0.030.54 ± 0.140.51 ± 0.160.42 ± 0.120.73 ± 0.16
Source emissionGasoline0.77 ± 0.10 a0.40 b0.22–0.55 d0.32 ± 0.17 a
Diesel0.73 ± 0.18 a0.43 c0.38–0.64 e0.37 g0.4–0.5 e
Wood0.84 ± 0.16 a0.62 c0.43 f0.42 ± 0.18 a
a US EPA 1999 [51]; b Rogge et al. 1993 [52]; c Manoli et al. 2004 [53]; d Simcik et al. 1999 [54]; e Sicre et al. 1987 [55]; f Li and Kamens 1993 [56]; g Grimmer et al. 1983 [57].
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Chimjarn, S.; Delhomme, O.; Millet, M. Temporal Distribution and Gas/Particle Partitioning of Polycyclic Aromatic Hydrocarbons (PAHs) in the Atmosphere of Strasbourg, France. Atmosphere 2021, 12, 337. https://doi.org/10.3390/atmos12030337

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Chimjarn S, Delhomme O, Millet M. Temporal Distribution and Gas/Particle Partitioning of Polycyclic Aromatic Hydrocarbons (PAHs) in the Atmosphere of Strasbourg, France. Atmosphere. 2021; 12(3):337. https://doi.org/10.3390/atmos12030337

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Chimjarn, Supansa, Olivier Delhomme, and Maurice Millet. 2021. "Temporal Distribution and Gas/Particle Partitioning of Polycyclic Aromatic Hydrocarbons (PAHs) in the Atmosphere of Strasbourg, France" Atmosphere 12, no. 3: 337. https://doi.org/10.3390/atmos12030337

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