Descriptive statistics for the observed pollutant concentrations is provided in
Table 4, while the obtained SHAP importance is provided in
Table 5. In addition to their use for air quality forecasting [
19,
85], machine learning models, when supplemented by explainable and model interpretability analyses, provide insight into the significance and impact of considered prediction variables. By applying deep SHAP analysis to NO
LSTM forecasting, García and Aznarte [
18] registered a significant influence of meteorological parameters on the modeled pollutant concentrations, which has been shown to be in compliance with the well-known natural phenomena in the investigated area. Further, Kang et al. [
86] have used SHAP analysis to investigate the seasonal impacts of meteorological factors on the spatiotemporal prediction of NO
and O
levels. In this study, we have made a step forward by analyzing the air pollutant behavior in a certain type of environment affected by different meteorological conditions and the presence of other polluting species.
To demonstrate the potential of the applied methodology, we provide details on the three most important predictors that describe the evolution of benzene concentration. The interrelations with toluene and finest aerosol fraction dominantly shape benzene concentrations, while other important variables include meteorological parameters temperature (T02M and TMPS), volumetric soil moisture content (SOLM), and momentum flux direction (MOFD), as well as concentrations of total nonmethane hydrocarbons (TNMHC) and total nitrogen oxides (NO).
5.1. Toluene
Although benzene and toluene most often appear as copollutants sharing the same sources (traffic, petrochemical industry, commercial product manufacturing, etc.), their reactivity and atmospheric half-life differ. Namely, toluene contains an electron-releasing methyl group attached to a benzene ring, which makes it more reactive and results in different environmental behavior of toluene and benzene, which can be indicative when distinguishing between emission sources.
The results have shown that benzene and toluene are strongly interrelated, with toluene levels affecting an average of 35% of the benzene concentrations and the decrease of 1.4
g m
relative to the expected levels (
Table 5). According to the findings, three types of environmental conditions that shape the benzene behavior depending on the toluene concentration range can be identified.
The first environment is characterized by toluene concentrations below 2
g m
(
Figure 4), as well as low concentrations of all pollutants including aerosol fractions, m, p-xylenes, and NO, except ozone, with the registered values exceeding 70
g m
. Within these conditions, the considerable variability of all analyzed meteorological parameters and diverse weather conditions were observed, which indicates consistent emission sources. Additionally, the obtained organic/inorganic gas relations and a toluene-to-benzene ratio above 2 (
Figure 4), suggests that the majority of low benzene concentrations assigned to this environment originate from evaporation processes related to petrochemical refinery sources in the southern zone of Pančevo, including equipment leaks from valves or steam power units and leakage during the transport.
The second environment refers to toluene concentrations ranging from 2 to 4.5 g m with no registered impact on benzene levels and SHAP values around zero. The belonging concentrations of NO were below 30 g m and above 100 g m, NO levels were below 100 g m and above 170 g m, while PM and TNMHC were below 64 g m and 110 g m, respectively. The observed extreme concentrations of nitrogen oxides, as well as relatively high concentrations of fine particles and lacking relationship between toluene and benzene all point to the strong and intermittent emission source, which can be attributed to HIP Azotara Pančevo, one of the most important regional plant of mineral fertilizers and nitrogen compounds, and agricultural practices on the surrounding farming areas related to heavy use of fertilizers and livestock waste.
Toluene concentrations ranging from 4.5 to 15
g m
describe the third environment, which appears to be favorable for elevating benzene concentrations (
Figure 4). Within the defined conditions, two subenvironments related to separate emission sources can be distinguished based on the benzene-to-toluene ratio.
The first subenvironment is characterized as highly affecting conditions responsible for driving the observed benzene concentrations up to 14 g m above the expected value. Thereby, the role of toluene seems to be of particular significance, since its relative impact on benzene concentrations increased to 55%. The high levels of benzene were accompanied by high PM, NO, and TNMHC concentrations, as well as ozone levels below 70 g m. Regarding meteorological parameters, the medium- and the highly-supporting environment was related to air temperatures below 15 °C, low wind speeds (below 2 m s), low planetary boundary layer height of 200 m, and high air humidity above 80%, all of which can be assigned to a cold period of the year. During autumn and winter months, these unfavorable meteorological conditions contribute to high concentrations of pollutants originating from fossil fuel burning for heating purposes. Additionally, reactions with photochemically produced hydroxyl radicals, which represent the principal mechanism of vapor-phase toluene and benzene atmospheric removal, are suppressed during the cold months, which results in the prolongation of pollutants’ lifetimes from a few days in the summer season to several weeks in autumn and winter.
The second sub-environment refers to conditions with a lower impact on benzene concentrations (up to 8
g m
) that govern high levels of benzene (>15
g m
), m, p-xylene (>14
g m
), and NO
(>40
g m
), and above average TNMHC levels (t). Concurrently medium to high air and soil temperatures, air pressure, and humidity, as well as a toluene-to-benzene ratio in the range between 1 and 2, can be attributed to the site-specific and year-round continuous contribution of traffic (
Figure 4) [
87].
5.2. Particulate Matter (PM)
The aerosol fraction PM
and benzene are interrelated in four environments, which define an average of 16.2% observed concentrations and lead to the average increase of about 0.6
g m
(
Table 5) in benzene levels. In the first case, the benzene concentrations exhibit a decrease by 1
g m
, in two of the identified environments benzene levels increase by 2.5
g m
, while the interrelationship with PM
in the last case does not seem to affect its levels (
Figure 5).
In the first environment, the reduction of benzene concentrations by 1
g m
is affected by a decrease in PM
concentrations to 20
g m
and complemented by low concentrations of atmospheric aerosols PM
and PM
(up to 30
g m
) and high concentrations of O
(above 70
g m
). The concentrations of toluene, TNMHC, and m, p-xylenes are observed in a wide range of values, which disables drawing conclusions on the relationship between particles and VOCs, however, the calculated toluene-to-benzene ratio above 2 suggests the dominant impact of the industrial evaporation processes in this environment [
88]. The observed pollutant levels have occurred under low atmospheric pressure, and medium or higher temperatures, planetary boundary layer height, humidity and momentum flux intensity, i.e., the atmospheric conditions that enable vertical mixing, pollutant dispersion and transport. Previous research has shown that, despite the constant pollutant emissions, PM levels could fluctuate up to several times with the change in influential weather variables [
89,
90]. Some studies have reported elevated PM concentrations under calm weather, mild wind and low planetary boundary layer height, temperature and relative humidity, while findings associating high PM levels with high wind speed and low humidity, or increased precipitations are also available. These contrasting results can be explained by the fact that aerosol water largely impacts complex heterogeneous gas/liquid/solid partitioning of freshly emitted particles and precursor gases.
Medium concentrations of benzene registered in the second environment were independent (SHAP values are zero) of PM levels ranging from 20 to 30 g m, and accompanied by moderate levels of PM, PM, and m, p-xylenes, and higher concentrations of toluene and NO. The prevailing conditions can be described by the average air humidity of 50%, air pressure of 1000 mbar, boundary layer height ranging from 300 to 500 m, and temperatures from 10 to 20 °C.
In the highly affecting environment, the increase of benzene concentrations by 2.5 g m was driven by the PM levels ranging from 30 to 92 g m, under the impact of temperatures below 10 °C, planetary boundary layer heights below 400 m, and medium or higher air pressure and humidity. These meteorological conditions and the toluene-to-benzene ratio below 1 correspond to the cold part of the year when the burning of fossil fuels can be considered the major cause of low air quality.
An additional interrelation pushes benzene levels by 1.5
g m
with the PM
concentrations exceeding 60
g m
, in the fourth environment, defined by higher concentrations of TNMHC, m, p-xylenes, all fractions of atmospheric aerosols, NO and NO
, and low O
levels. The atmospheric conditions, which can be attributed to the cold part of the year, including low wind speed, temperature, and planetary boundary layer height (up to 2 m s
, 10 °C and 400 m, respectively), medium and high air and soil humidity, and high air pressure, created the unfavorable environment for the production of secondary pollutants, which explains the lower concentrations of O
, while slightly higher toluene-to-benzene ratio values equal or above 1 indicates the contribution of traffic emissions to high pollutant concentrations during autumn and winter season [
91].
5.3. Temperature
Temperature is recognized as the third important parameter that shapes 15.8% of benzene levels, lowering its concentrations by about 0.5
g m
on average. Its impact is complex but relatively symmetrical and monotonically decreasing with increasing temperature, with a pronounced positive effect at temperatures lower than 9 °C and a negative effect at temperatures higher than 14 °C (positive/negative effect refers to an increase/decrease of benzene concentrations),
Figure 6.
Within the range of lower temperatures, two environments have been identified. In the first case, the benzene concentration increase up to 1 g m is followed by low to medium concentrations of toluene (2 g m on average), m, p-xylenes (5 g m on average), nitrogen oxides (25 g m on average) and all atmospheric aerosol fractions, low concentrations of O, as well as high cloudiness and intensity of momentum flux, low insolation and air pressure, and a very low planetary boundary layer height of 350 m.
In the second environment, which can be assigned to fossil fuel burning for heating purposes during the cold season, benzene levels increase almost linearly with the drop in temperature by 2.3 g m on average. The increase is followed by high concentrations of aerosols, nitrogen oxides, and benzene (above 12 g m for the latter), extremely low concentrations of O (below 20 g m), stable atmospheric conditions, low temperature, and planetary boundary layer, but high pressure and air humidity.
As shown in
Figure 6, interrelations between benzene and temperature, which ranged from 9 to 14 ºC, were apportioned in three subenvironments. In the first case, a positive impact of temperature was accompanied by an increase in benzene concentrations and lower levels of toluene (2.5
g m
on average), medium levels of m, p-xylenes (5
g m
on average) and NO
(38
g m
on average), and medium boundary layer heights. Contrary, in the second case, temperature impact reduces to a minimum while the environment is characterized by an increase in the pollutant concentrations, approximately 25%, 35%, and 52% for VOCs, NO
, and all particle fractions, respectively. Under these conditions, the elevation of SHTF for 680%, downward short-wave radiation flux (DSWF) for 54%, and LHTF for 26% was observed, while soil moisture (SOLM) and low cloud cover (LCLD) declined for 7% and 28%, respectively. Ambiances with higher PM concentrations and gaseous pollutants have been associated with ambivalent impacts on the surface temperature while an increase in water vapor induces a rise in the shortwave cloud radiative forcing [
92]. In addition, SOA formation from precursors such as particles, NO
and dominantly the benzene homologs, toluene, and xylene, is enhanced in the presence of water vapor with NO
being the most soluble species. Prevalent temperature values in described subarea are not sufficient to render photolysis of VOCs. In the third subarea, when temperature impact is negative, the ambiance is shaped by a decrease of benzene and even higher levels of pollutants (more than 50, 40, and 80% for VOCs, NO
, and PM, respectively). Much of the anticipated energy balance concept in the land–atmosphere interactions rely on soil moisture as a key variable. The content of soil moisture depends on atmospheric conditions such as precipitation, radiation, and evaporation, which further alters surface turbulent and radiative heat fluxes. Some studies witnessed that low precipitation suppressed the availability of soil moisture causing a decrease in latent heating (LHTF) and an elevation of sensible heating at the surface (SHTF). These conditions, accompanied by increased temperature, affect atmospheric thermodynamics and the structure of PBL and make the atmosphere less suitable to maintain deep convection. Causality in the coupled land/surface–atmosphere system becomes more complicated in the presence of atmospheric pollutants and variations of local meteorological conditions. For example, suspended particles scatter shortwave radiation and trap longwave radiation to a different extent, which could modify surface temperature and heat fluxes [
92].
In the environment with temperatures above 14 °C, benzene concentrations, lower up to 1.5 g m on average, are accompanied by higher concentrations of PM, NO, m, p-xylenes and TNMHC, as well as by low humidity, higher air and soil surface temperatures, and planetary boundary layer heights above 1200 m. In addition to this, the toluene-to-benzene ratio over 3, reflects the industrial activities at the regional chemical plant Azotara Pančevo, which manufactures nitrogen chemicals and mineral fertilizers, but also soil preparation, maturing, and other farm production processes in the surrounding agricultural land during the spring and summer season. Besides, meteorological conditions in the warm season are favorable for benzene removal. In the troposphere, photolysis transforms VOCs or they react with OH and radicals and O. Concerning the reaction rates with the OH radical, which is a dominant loss of most VOCs, lifetimes of benzene, toluene, and xylenes in the air are up to 10 days, 2 days, and 6 hours, respectively, while their presence is up to several years regarding loss by NO radical and O. In the presence of sunlight, the reaction between VOCs and •OH yields a peroxy (•HO) and an alkyl or substituted alkyl radical (•ROO). Such produced radicals further react with NO, converting it to NO, which photolysis forms O. As evident from the presented simplified chemical mechanisms, a photo equilibrium between NO, NO, O, and kinetic reactivity of radicals and VOCs lead to no net formation or loss of O. The VOC/NO, ratio impacts the production of O as follows: (i) the occurrence of NO, sinks (NO-limited conditions) lowers the amount of formed O, and (ii) during VOC-limited conditions, a net formation or loss of OH radicals leads to an intensification or reduction of overall reactivity of all presented VOCs.