The average annual B[a]P concentrations of 3.73
and 2.78
in 2018 and 2019, respectively (
Table 6), significantly exceeded the European Directive set level of 1
. The maximum pollutant level reached 43.71
in the first year of the study period. At the same time, no values exceeded the critical threshold for the concentration of PM
, As, Cd, Ni, and Pb, and inorganic gaseous pollutants.
As indicated by the mean absolute SHAP values, the temperature at surface (TMPS), As, PM
, and total nitrogen oxide (NOx) concentrations appear to be major factors for governing B[a]P environmental fate (
Table 7). In addition, the most important variables also include NO, SO
, Pb, and Cd concentrations, as well as the temperature at 2 m (T02M) and momentum flux intensity (MOFI)m have been shown to affect B[a]P dynamics. However, for this paper, we will focus on the aforementioned four.
5.1. Temperature at Surface
In this study, the temperature at the surface (TMPS) was estimated to be the most important parameter responsible for the B[a]P concentration increase of 1.17
on average, while mutual interrelations between TMPS and other studied parameters define three types of environmental conditions being responsible for shaping B[a]P levels. As a high-molecular-weight PAH, B[a]P is dominantly particle-bound in the atmosphere. The B[a]P partition between gas and particles is enhanced during colder months due to low temperature and high atmospheric pressure, which cause intense descending air movements and dry deposition of organic compounds [
74]. Additionally, previous studies have shown that higher organic carbon content of particles in the cold season negatively affects the immobilization and biodegradation of PAHs [
75], while high temperatures and light intensity in warm months enable both their photo- and biodegradation.
The first type of environment resulting in the increase of B[a]P concentrations up to 3.4
(
Figure 7), was characterized by medium to low PM
, B[a]P, As, Cd, and Ni levels (35.2
, and 3.4, 1.4, 0.3, and 2.5
on average, respectively), medium to high NO and NOx concentrations (6.9 and 23.4
on average, respectively), and meteorological parameters registered in a wide range of values. The observed constancy of the conditions suggests that this environment type might be related to anthropogenic sources, such as traffic and off-road vehicles.
In the second type of environment, TMPS was ambivalently related to the B[a]P concentrations, leading both to their decrease by up to −1
and the increase by up to 0.7
. Compared to the first type, the second type of environment was characterized by lower B[a]P, As, Cd, Ni, Pb, PM
, NO
, and SO
(2.0, 1.1, 0.2, 1.8, 3.8
, and 32.8, 13.8, and 13.4
, respectively) and higher NO and NOx (about 9.5 and 28.8
, respectively) mean concentrations. The decrease in temperature range and wind speed (
Figure 7) and the rise in relative humidity, alongside other meteorological parameters (MOFI, LIDS, and SHIF), indicate the stability of the atmosphere and cold weather-related conditions.
The third type of environment, leading to a decrease in B[a]P concentrations of 2.3
, was associated with medium mean PM
, SO
, and As levels (34.6 and 14.1
, and 1.6
, respectively), maximum observed B[a]P, As, and NO
concentrations (43.7 and 13.6
, and 98.5
, respectively), standard lifted index (304), and relative humidity (98%), minimum study period temperature (−15.3
C), as well as the highest number of precipitation events, i.e., non-zero TPP6, CPP6, and CRAI values (
Figure 7).
The atmospheric stability and the intensity of anthropogenic emissions during the cold part of the year seem to result in high B[a]P concentrations. Since PAHs are mostly particle-bound, and precipitation scavenging plays a significant role in the PM removal from the atmosphere, it could be expected that wet deposition represents a way of PM-bound B[a]P elimination from the atmosphere. As shown by Liu et al. [
76], wet removal and photodegradation are up to 10 and 5 times, respectively, more efficient in B[a]P elimination during summer than in winter. Additionally, wet scavenging dominates as a B[a]P removal path in summer, while the impact of photodegradation outweighs the wet removal in winter.
5.2. Arsenic
This study suggests that As concentrations affect B[a]P level dynamics up to 0.9
on average (
Table 7), more than any other pollutant. A few types of environment were distinguished by analyzing the interrelations between As and B[a]P and their coexistence within certain conditions.
The obtained interrelation indicates similar emission sources of inorganic As, in a mixture of arsenite (AsIII) and arsenate (AsV), and organic B[a]P in the air, that could be identified as high-temperature combustion of fossil fuels and wood [
77,
78]. In addition, because of low volatility, both As and B[a]P mostly exist as particle-bound in the atmosphere, particularly associated with fine aerosol fractions. Up to approximately 10% of B[a]P occurs in the gaseous phase [
79], although the multiphase B[a]P distribution was also highly dependent on ambient temperature [
80].
In the first type of environment, B[a]P concentrations exhibited an increase in the range from 4 to 7
(
Figure 8), with maximum concentrations reaching 30
. The relative impact of As, i.e., its association with B[a]P, compared to other studied parameters, reaches a maximum share of 43.6%. This environment was characterized by the lowest As and Cd concentrations, below 2 and 1.5
, respectively, and low to medium NOx, SO
, and PM
levels of below 55
, below 25
, and from 10 to 25
, respectively. Other PM-bound constituents, including Ni and Pb, were registered in higher concentrations of 8.2 and 24.6
, respectively, which suggests the impact of local anthropogenic source emissions and dust resuspension, as well as the impact of occasional fossil fuel burning emissions. The co-occurrence of As and B[a]P was observed in the wide range of temperatures at the surface and 2 m (from 1 to 20
C), which indicates that the relationship between As and B[a]P concentrations was not seasonally dependent. Additionally, this type of environment was featured by PBLH below 150 m, humidity above 74%, wind speed below 2 m s
, and very low MOFI (
Figure 8), all of which reflected extremely stable meteorological and atmospheric conditions, which were registered on a few occasions during the measurement campaign. Therefore, it can be assumed that in the first type of environment, the contributions of remote air pollution sources and atmospheric long-range transport to the observed B[a]P and As concentrations can be excluded.
The second type of environment was characterized by an increase in B[a]P concentrations up to 4
on average and by the lower impact of As (5 to 20%), relative to other pollutants. In comparison to the previous one, this environment was also marked by up to three times higher PM
levels (70
), up to two times higher As (5
) and NOx (up to 100
) levels, and somewhat higher SO
(30
) concentrations. The assigned meteorological conditions included low humidity, air and soil temperatures ranging from −5 to 20
C, PBLH below 480 m (
Figure 8), and wind speed below 3.7 m s
, as well as MOFI values typical for the cold season. As can be concluded, the second type of environment represented the cold season and its associated emissions of As and B[a]P as well as inorganic oxides from heating-related sources. In cold weather conditions, PM, NOx, SO
, and As are slow-reacting and the atmospheric reactions associated with the generation of secondary air pollutants (other oxide forms, sulfates, nitrates, or ozone), reaction byproducts or fine particles require a prolonged time, which in this case contributed to high pollutant concentrations assigned to the second type of B[a]P environment.
The third type of environment referring to the majority of measured pollutant concentrations recognized more than one pattern of As-B[a]P interrelations. Depending on the wind speed and other meteorological factors, both high and low B[a]P and As concentrations were registered. Namely, wind speed below 2 m s was associated with the highest pollutant concentrations, while the increase in wind speed above 5 m s resulted in a significant decrease in both pollutant concentrations below 1 . These findings suggest a negligible contribution of regional pollutant sources to air quality at the sampling site, but also the presence of local pollution sources and processes, such as resuspension of ash from crude-oil and lignite-fired boilers, which strongly affect pollutant concentrations during the episodes of low wind speed.
SHAP values ranging from −0.6 to 0 referred to the situations in which As levels had a moderately negative or null impact on B[a]P dynamics. On these occasions, As, B[a]P, and PM levels were very high, 13.6 , 22 and 177 , respectively, while the SO and NOx levels did not exceed 10 . Given these findings were associated with the T02M range from −3 to 5 C, we can assume that As and B[a]P have separate sources during the cold season, which contribute to high concentrations of either one or another pollutant. More data and further analysis could provide detailed insight and confirm these assumptions.
5.3. Particulate Matter
The PM concentration is the third significant parameter that affects B[a]P concentrations, as shown by the mean absolute SHAP value of 0.8 . In the absence of meteorological conditions favoring the association of B[a]P and small particle fraction, the relationship between PM and B[a]P stands out.
The highest observed positive associations between PM
levels and B[a]P concentrations, in compliance with a relative share of 57.52% and assigned an absolute SHAP value of 8.36
, was registered in the environmental conditions associated with the lowest concentrations of all pollutants, including PM
levels below 32
. As regards meteorological conditions, the strongest interrelation between PM
and B[a]P concentrations was detected in the environment characterized by air and soil temperatures ranging from 0 to 20
C and low wind speed (below 2 m s
). This type of environment is not seasonally specific and might indicate natural interactions in the atmosphere such as associations between PAHs and PM. Atmospheric PAHs such as high-ring B[a]P are easily adsorbed onto suspended particles with high organic content [
76] while the degradation of particle-bound B[a]P fraction is minimized or inhibited. The gas-to-particle partitioning of pollutants and atmospheric removal by wet scavenging are favored depending on the atmospheric conditions, PM surface, its composition and size, and contaminant properties [
81]. In the warm season, the increase in temperatures leads to increased B[a]P volatility, followed by its biodegradation. As the impact of PM
on B[a]P levels weaken the environmental conditions change slightly towards higher pollutant concentrations and an increase in wind speed and PBLH (
Figure 9).
Given the SHAP value of −0.87 PM
, a high number of registered medium to high B[a]P concentrations was negatively associated with PM
, particularly in the environment of high suspended particles As and low Cd, Ni, Pb, NOx, and SO
levels. As regards meteorological conditions, these interactions took place during the coldest days of the winter period, when low PBLH, high cloudiness, and wind speed up to 3 m s
were recorded (
Figure 9).
As previously mentioned, the cold season was the period of intense emissions from power plants, domestic heating units, and commercial sources, resulting in elevated levels of PM, especially those of smaller diameter (PM
and PM
) rather than PM
. The finest particle fractions represented a highly suitable matrix for the adsorption of PAHs and these associations could be a possible explanation for the negative relation between B[a]P and PM. A number of studies have shown that small particle diameter plays an important role in the entrapment of PAHs, and thus more than 70% of high-molecular-weight PAHs with higher octanol-water partition coefficients, including B[a]P, is PM
-bound [
82,
83]. Low air temperature, wind speed, solar radiation, and PBLH inhibited the vertical diffusion of pollutants and enhanced gas-to-particle pollutant partitioning [
84,
85]. In addition to this, the strong adsorption capacity of fine PM fraction prevailed over other environmental factors and suggests the particle partition of B[a]P to PM
and a smaller fraction rather than to PM
. Lobscheid et al. [
86] used multivariate linear regression models to predict relations of ambient B[a]P levels and PM
concentrations, spatial, temporal, and meteorological variates. The most significant variables included the average daily PM
concentration, wind speed, temperature, and relative humidity.
In contrast to this, during the warm and windy season, when the average temperatures, wind speed, and PBLH exceeded 15
C, 4 m s
, and 450 m, respectively, the concentrations of PM
and their constituents exhibited a significant decrease, although the same does not apply for NOx and SO
. High solar radiation and temperature in warmer seasons lead to the dispersion and photochemical degradation of the majority air polluting species [
80,
87], but the persistence of medium to high gaseous oxide levels during the warm season indicated the impact of intense and year-round continuous traffic emissions at the sampling site.
5.4. Nitrogen Oxides
Similar to PAHs, NOx (NO and smaller share of NO
) emissions mainly resulted from the high-temperature combustion processes in power plants and motor vehicles. Both groups of compounds, PAHs and NOx, were subject to photochemical reactions in the atmosphere. Besides undergoing gas-particle phase distribution, PAHs are precursors for the generation of nitro-compounds. Namely, in the presence of free radicals, OH-PAH or NO
-PAH are formed and subsequently, in the few-hour reaction with NO
upon release of nitric acid or water molecule, nitro-PAHs were generated [
88,
89].
The mean absolute SHAP value of 0.6
defines NOx as the third most significant parameter for shaping B[a]P levels in two distinguished types of environment, one of which strongly supports the increase in B[a]P concentrations. The polluted environment, with moderate to high B[a]P levels (average value of 3
) and attributed SHAP value of 6.78
, was characterized by a wide range of NOx, PM
, and SO
concentrations, from 1.28 to 144
, up to 70
and up to 30
, respectively; however, the lowest levels of PM-bound As, Cd, Ni, and Pb (
Figure 10).
The meteorological conditions which enabled the positive impact of NOx on modelled B[a]P level dynamics and a wide range of B[a]P, NOx, PM
, and SO
concentrations, refer to stable high-humidity cold weather without precipitations, with wind speed and PBLH below 3 m s
and 400 m, respectively; temperatures in the range from −7 to 20
C, as well as with the corresponding CAPE, CPP6, CRAI, MOFI, and SHIF values (
Figure 10). Under these conditions, common emission sources (fossil fuel burning for heating purposes) of the listed pollutants were intensified leading to their higher concentrations. In addition, the stagnant high-humidity conditions during heavy haze events enhanced the transformation of primary emitted particles containing PAHs to secondary organic aerosol (SOA), with the prominent presence of sulfate and nitrate water-soluble species dissolved in an aqueous outer particle layer [
90].
The majority of studied pollutant events can be distinguished into two groups depending on the SHAP values and the strength of NOxs negative impact on modeled B[a]P concentration dynamics. The type of environment in which NOx and B[a]P interrelations are expressed by a lower SHAP value of −1.76
, refers to the warm season, with air temperatures from 15 to 20
C, an occasional wind of high speed from 5 to 8 m s
and mean daily PBLH above 1000 m. As can be expected, these meteorological conditions have favored pollutant dispersion and resulted in low pollutant concentrations, as confirmed by measurements (
Figure 10). During the warm season, PAHs undergo photolysis or processes which can yield their derivative compounds, such as oxygenated and nitrated PAHs. The UV-mediated ozone photolysis is a source of OH radicals in the troposphere, which react with PAHs to produce intermediate compounds OH-PAHs. After substitution with NO
, OH-PAHs are further converted to nitro-PAHs, particularly at night, when the concentrations of NO are low [
88]. Additionally, nitro-PAHs are also generated in the chemical reactions between PAHs and NO
-radicals, originating from reactions between O
and NO, and their formation can explain the negative NOx and B[a]P interrelations.
The SHAP value of −0.3 was attributed to the environment where no significant interactions between NOx and B[a]P were registered. Occasionally, these events were characterized either by high concentrations of B[a]P, PM, PM-bound constituents, and low NOx levels, or the opposite, the lowest concentrations of suspended particles, their constituents and high NOx levels exceeding 50 , which implies two different sources of origin.