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Article

Pollution from Highways Detection Using Winter UAV Data

1
Institute of Environmental Engineering, Peoples’ Friendship University of Russia (RUDN University), 6 Miklukho-Maklaya Street, 117198 Moscow, Russia
2
V.V. Dokuchaev Soil Science Institute, Pyzhevsky St., 7, 119017 Moscow, Russia
*
Authors to whom correspondence should be addressed.
Drones 2023, 7(3), 178; https://doi.org/10.3390/drones7030178
Submission received: 1 February 2023 / Revised: 23 February 2023 / Accepted: 2 March 2023 / Published: 6 March 2023
(This article belongs to the Special Issue Ecological Applications of Drone-Based Remote Sensing-II)

Abstract

:
This study identified and evaluated the association between metal content and UAV data to monitor pollution from roadways. A total of 18 mixed snow samples were collected at the end of winter, utilizing a 1 m long and 10 cm wide snow collection tube, from either side of the Caspian Highway (Moscow-Tambo-Astrakhan) in Moscow. Inductively coupled plasma optical emission spectrometry (ICP-OES) was used to examine the chemical composition of the samples, yielding 35 chemical elements (metals). UAV data and laboratory findings were calculated and examined. Regression estimates demonstrated the possibility of using remote sensing data to identify Al, Ba, Fe, K, and Na metals in snow cover near roadways due to dust dispersal. This discovery supports the argument that UAV sensing data can be utilized to monitor air pollution from roadways.

1. Introduction

Dust contains a variety of chemical compositions because it originates from a variety of sources, including the climate, human activities, soil particles and rocks, pollen, hair, clothing fibers, bacteria, dust mites, bits of dead bugs, microscopic specks of plastic, plant materials, and dander (dead skin cells shed by animals) [1,2,3]. According to ref. [4,5,6], road and air dust is a complex particle mixture that has the potential to transport high concentrations of different contaminants, such as metals, hydrocarbons, nutrients, particulates, de-icing salts, and mold spores, which may result in a major source of atmospheric air pollution through resuspension by wind and vehicular movements. According to ref. [7], the chemical composition and particle size of dust are crucial when assessing the consequences, and they vary across distance and time. Ref. [8] found that meteorological circumstances, the soil environment, bedrock, and human activities all substantially impacted the diversity of street dust composition. According to ref. [9], road dust is a complex combination of particles and pollutants originating from a wide range of urban, automotive, and industrial sources and activities, and its components and quality are indications of environmental pollution in big cities. Metals from atmospheric deposition can accumulate in dust by sedimentation, impaction, and interception [10]. Furthermore, metal concentrations in crops are determined by the metal content of soil and crop absorption capabilities [11], which are also directly related to soil properties such as soil organic matter [12], pH, salinity [13], and heavy metal morphology [14].
Levels of elements, particularly toxic elements, linked with non-physiologically regulated anthropogenic activities may vary depending on geographic and geochemical settings and land-use activities. The elemental composition of hair samples may reflect this, indicating environmental pollution or hot zones [15]. Metal contamination in the soil might pose an ecological problem. Cd and Hg were discovered to pose the greatest potential ecological concerns [16,17]. Metal-polluted food causes substantial health concerns to local populations, including Itai-itai disease [18] and even cancer [19]. As a result, [20], a research study demonstrated the mutuality of the close relationship between the metal contents of dust deposits and topsoils. Ref. [21], for example, analyzed possible ecological and human health risks posed by heavy metals in soil rather than in crops, let alone their link. Exposure to these metals may have several health repercussions for this or future generations. Acute or chronic exposure to these metals has been linked to the genesis of many illnesses. Lead, for example, has been linked to anxiety, arthritis (rheumatoid and osteoporosis), attention deficit disorder, blindness, cardiovascular disease, cartilage destruction, constipation, depression, epilepsy, gout, immune repression, infertility, kidney disorder, liver dysfunction, menstrual problems, muscle weakness, spinal cord pathology, peripheral neuropathies, psychomotor dysfunction, sudden infant death syndrome, and many other conditions [22,23]. Furthermore, metals in soil can endanger human health in three ways: inhalation, dermal absorption, and soil ingestion [24]. In most circumstances, children are more vulnerable to metal contamination than adults [25]. As a result, several researchers have focused their efforts on the human health risks posed by metals in soil [26]. Previous research employed remote sensing to monitor and map marine pollution as well as investigate the relationships between metals, soils, and crops, with a particular emphasis on metal distribution and bioaccumulation. Ref. [27] utilized the combination of satellite data and UAV technology to explore the continuity of climatic and human changes in the Alps and, more extensively, on animals, biodiversity, and ecosystems in mountain and wilderness settings. The emphasis of the study was to support decision-makers involved in wildlife and domestic animal management and planning (both hunting and pastoral) as well as public health (from the perspective of One Health). Ref. [28] employed remote sensing to map oil pollution, suspended solid contents, algae blooms, and floating plastic debris in marine waterways via absorption. Ref. [29] demonstrated that data on meteorological conditions, including light pollution, can be acquired across a long vertical range (up to tens of kilometers); however, the placement of the vertical profiles was reliant on the air circumstances (mainly winds). Despite this accomplishment, tower measurements are confined to a single location and height or different heights of the same tower. Ref. [30] reported the use of remote sensing to model the relationship between predictor variables during the cross-validation process for both non-imaging and imaging sensors for clay, sand, and SOM, which are crucial in tropical soil management. Ref. [31] demonstrated the use of remote sensing for quantitative (spectral-based) soil property assessments. Unfortunately, only a few studies have employed remote sensing or UAV data to investigate the dust contamination of roadside snow. It is thus worthwhile to investigate the relationship between dust, its metal content, and snow and collect remote sensing and UAV data to monitor snow pollution.

2. Materials and Methods

Gritchino in Moscow Oblast, Russia, was chosen as the test site because of several variables, including the composition of traffic flow along the Caspian Highway (Moscow-Tambov-Astrakhan), which runs through large agricultural areas used for wheat and maize cultivation. Vehicular movement on the route had increased to over thirty thousand vehicles by 2020 [32], with traffic intensity on the route increasing more than five times since its completion in 1983. The site is located at (54°, 36°, 15°) North and (38°, 6°, 20°) East. It has a mild continental climate with warm summers and cold winters dominated by western or southwestern winds [33]. The major wind direction for the winter of 2021/2022 was southwest, according to the Kashira meteorological station records. The average temperature in February was −10 °C. The road is flanked on both sides by fertile land [33].
Snow samples were collected at a distance of 30–190 m from both sides of the Caspian Highway (Moscow–Tambo–Astrakhan) at the end of winter 2021–2022, according to the snow sampling procedure (stratified sampling procedure) described by ref. [34]. The locations of the sampling stations were calculated using UAV parameters obtained throughout the sampling campaign, with an error of less than 10 cm. A total of 18 mixed samples (three samples were mixed at each test point) were collected using a snow collecting tube 1 m in length and 10 cm in diameter, as illustrated in Figure 1. Each sample’s snow depth was measured. The samples were subsequently taken to Moscow’s V.V. Dokuchaev Soil Science Institute for processing and chemical analysis. Once 90% of the sample had melted, it was de-iced at room temperature and chilled to finish the melting process. The samples were subsequently filtered using polycarbonate filters with a pore size of 0.45 μm and diameter of 47 mm to separate the water and particles for analysis using inductively coupled plasma optical emission spectrometry (Agilent 5800 ICP-OES). Dust particles were digested into solution using nitric acid before being injected into the plasma. This was performed to bring the entire dissolved solid concentration into the instrument’s operating range, thus lowering the detection limit of the technique. To allow any reaction gases to escape, the samples were allowed to stand for 10 min after 2 mL of strong nitric acid reagent was applied to each sample [35].
The samples were then treated with 6 mL of concentrated hydrochloric acid (SG 1.18) for another 10 min. To prevent the production of insoluble chloride salts, nitric acid was added first, followed by hydrochloric and hydrofluoric acids. The samples were subsequently heated in line with EPA Procedure 3051 in a Milestone Ethos microwave system. The samples were then heated to 175 °C for 10 min, kept between 170 and 180 °C for another 10 min following the microwave digestion procedure, and cooled for 5 min. The sample containers were transferred to a fume closet to achieve room temperature. To obtain a homogenous sample, the volume of the digest was increased with distilled water and then forcefully shaken in a 100 mL volumetric flask. The samples were allowed to settle overnight to remove any suspended solids [35]. A total of 35 chemical elements (metals) were identified. The findings of each sample were recalculated per m2 of dust particles, per m2 of melted water (without dust), and per snow mantle on m2 of soil surface.
UAV images were captured concurrently with the snow sample program using a DJI Matrice 200 quadcopter. A Zenmuse X4S FC6510 20 MP camera placed on a gyrostabilized suspension was used for visible spectral range (RGB) photography.
The DJI Go4 app was used to calibrate the UAV, while the Drone Deploy app was used for general flight tasks and camera setup on the Zenmuse X4S FC6510 (see Appendix A). The drone was flown at an altitude of 60 m with an average speed of 12 m/s. The flight plan was manually predefined, with a distance of approximately 30 m between neighboring passes (conventional serpentine flight patterns) and the nadir (0°, or perpendicular to the ground) camera view angles for generating point clouds. The image overlay between passes was set to 30%.
The Drone Deploy app automatically generated a flight path and capture mode based on the model of the quadcopter and camera, the specified flight altitude, and image overlap. The shots were taken from a height of 74 m.
The airborne survey yielded georeferenced photos in JPEG and TIFF formats.
The collected aerial pictures were analyzed using Agisoft Metashape Professional, a photogrammetric program. The software can handle images in visible (RGB), infrared, and monochrome spectral regions. The parameters supplied in each photograph’s metadata were utilized for this purpose.
Individual photographs with similar overlaps were stitched together using Agisoft Metashape. We obtained textured 3D terrain models in PDF, georeferenced in WGS 84 (EPSG: 4326), textured orthophotos, and digital terrain and relief models in various formats (JPEG, TIFF, KML, KMZ) from the aerial survey data processed by Agisoft Metashape. The obtained aerial survey materials and their processing were of high resolution. The resolution of the Zenmuse X4S FC6510 was 1.99 cm/pix, while the digital terrain model was 7.83 cm/pox.
Each pixel in the generated UAV photographs had a 24-bit color domain with three values: red, green, and blue (ranging from 0 to 255). The color separation for each pixel was achieved using the ILWIS v.3.3 standard option. The image’s red, green, and blue values were immediately extracted. One of the following formulas was used to retrieve more color images as shown in Table 1:
Red, green, and blue values ranged from 0 to 255, while hue, saturation, and intensity values ranged from 0 to 240, which complied with the Windows color scheme definition. In the formulas for hue, saturation, and intensity above, multiplication factor 240/255 was used to obtain that range.
Stata Standard Edition software for Windows 64-bit x86-64 was utilized. Correlation and regression analyses were performed to determine the nature of the relationship and the significance level between the metal content of the snow and the UAV-derived indicators (values of different colored images). Split validation and methodological concepts were used to forecast the fitness of the model used in the study (Licensed Microsoft Excel, Professional Plus 2019). Variables were split 60/40 for hypothetical testing. The predictions and coefficients of the models were similar to the technique utilized, demonstrating the validity of the approach and findings [36,37]. The sequence of the study is depicted in Figure 2.

3. Results

3.1. Metal Content in Water

Table A1, Table A2, Table A3 and Table A4 present data on the concentrations of metals in water, dust particles, and snow as well as the acquired UAV parameters, respectively. According to these findings, the concentrations of metals such as B, Cd, Ce, Co, Cr, Gd, and Ho in water were extremely low. The most abundant elements included Al, Ca, Fe, K, Mg, Na, and Zn. The levels of visible metals in water at the sampling location nearest to the road were distinguished by their greater amounts. As a result of the visual examination, the distribution of several components in water varied with the distance from the road.
There was a strong positive correlation between metal content and the UAV parameters (blue_av, gray, green, intensity, and red) in water. Meanwhile, the hue parameter had a weak relationship with metal content. Specifically, the strong positive relationship implied that the metals were extensively diffused in water. Overall, the predominant metal in water was Na, followed by K, Fe, and Al. On the contrary, the metal content exhibited a negative correlation with the cyan, magenta, saturation, and yellow parameters in water, with correlation coefficients of 0.38 (Al), 0.30 (Fe), 0.39 (K), and 0.46 (Na). The correlation coefficients for UAV parameters are shown in Table 2.
At a level of significance, Al and Fe metals demonstrated a linear regression association with the red parameter. On the other hand, K and Na had the best regression relationships with the intensity parameter. Overall, the synergistic and antagonistic impacts of the associated factors on metals in water were mostly focused on Al and Fe metals with red and K and Na metals with intensity. The red parameter, in particular, had a synergistic influence on the absorption of Al and Fe metals, whereas the intensity parameter exhibited antagonistic effects on the absorption of K and Na metals. Furthermore, levels of Al and Fe were significantly higher on the east side of the road than on the west side, compared to K and Na levels. This showed their extensive geological history. The elevated quantities of metals in water at the road’s edges might well be attributed to runoff water from de-icing treatments and asphalt pavement agents. Figure 3 displays the visual distribution of metals in water according to their associated characteristics. The regression coefficients for parameters are shown in Table 3.

3.2. Metal Content in Dust

  • The most abundant metals were Al, Ca, Fe, K, Mg, Na, and Pr. The increased levels of metals in dust at the nearest sampling stations were a distinguishing feature. Using remote sensing to detect metals in fresh snow was unlikely to be successful unless in a heavily contaminated region. Based on the relationships, several metals, such as Al, Ca, Ce, Co, Cr, Cu, Dy, Er, Fe, K, La, Li, Mg, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn, highlighted the importance of dust in monitoring roadside pollution.
  • There was a significant relationship between metal content (Al, Ca, Ce, Cr, Cu, Dy, Er, Fe, K, La, Li, Mg, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn) and the UAV parameters (blue av, gray, green, intensity, and red). Meanwhile, a weak correlation was observed with the hue parameter. The high positive association was an indicator of metal diffusion in dust. On the other hand, Al, Ca, Ce, Cr, Cu, Dy, Er, Fe, K, La, Li, Mg, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn metals in dust exhibited a negative association with the magenta, cyan, saturation, and yellow parameters. Table 4 depicts the correlation coefficients for the metal content of dust with the UAV parameters.
Metals Al, Ca, Ce, Cr, Cu, Dy, Er, Fe, K, La, Li, Mg, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn revealed a significant linear regression relationship with the red parameter. Overall, the synergistic effects of the UAV parameters on metals in dust were mostly concentrated on Al, Ca, Fe, K, and Na. Furthermore, the red parameter had a synergistic effect on the absorption of all metals along the road’s edge. This was evidenced by the higher levels of Al, Ca, Fe, K, and Na metals predominantly on the east side of the road compared to the other metals in dust. The increased levels of metals at the road edges might be due to the resuspension of asphalt pavement chemicals and runoff water from de-icing treatments. Figure 4 displays the visual distribution of metals in dust according to their associated characteristics. The regression coefficients for parameters are shown in Table 5.

3.3. Metal Content in Snow (Water and Dust)

Compared to prior approaches, data from remote sensing has proven to be a superior tool for monitoring pollution along roadways in a cost-effective and ecologically acceptable manner. Furthermore, according to ref. [38], the most efficient detection of contaminants in snow is sensor-based monitoring with spatial information (GIS). This discovery verified the ability of remote sensing to identify elemental metals such as Al, Ba, Fe, K, and Na in snow.
The concentrations of metals (Al, Ba, Fe, K, and Na) and UAV parameters (blue av, gray, green, intensity, and red) in snow had a substantial positive association. However, the hue parameter had a weak relationship with metal content. The substantial positive association suggested that the metals were widely distributed in snow. Overall, Na was the most abundant metal in snow, followed by K, Fe, Al, and Ba. On the other contrary, the metal content exhibited a negative association with the cyan, magenta, saturation, and yellow parameters in snow. The correlation coefficients for the UAV parameters are shown in Table 6.
The metals Al, Ba, and Fe in snow demonstrated the best regression with the red parameter, with P-values of 0.032 (Al), 0.008 (Ba), and 0.011 (Fe). K and Na metals, on the other hand, displayed a positive relationship with the intensity parameter. Similar to metal characteristics in water, the synergistic effects of the UAV parameters on metals in snow corresponded to the red parameter and were mostly focused on Al, Ba, and Fe metals. Furthermore, the red parameter had a synergistic effect on the absorption of all metals along the road’s edge, whereas the intensity parameter exhibited antagonistic effects on the absorption of K and Na metals. This was demonstrated by higher concentrations of Fe, followed by K, Na, Al, and Ba metals on the east side of the road compared to the west side. The obvious distinctive factors in the detection of metals in snow, similar to water, were the level of contamination and the UAV parameters with the most synergistic impact. In the case of this study, the red parameter had the greatest impact.
The presence of dust in the snow demonstrated the high degree of pollution found. Figure 5 displays the visual distribution of metals in snow based on their associated factors. The regression coefficients are shown in Table 7.

4. Discussion

4.1. The Influence of Roadways on Metal Dissemination

Several scientists have demonstrated that the influence zone of dust is approximately 150–180 m from the road [39,40], but the zone was spatially different for various metals in our case. The distribution maps of metals in snow that we acquired typically indicated that the road impact zone was approximately 30 to 90 m, which was less than the impact zones estimated by standard field methods [41]. This was most likely because the width of the impact zone is proportional to the intensity of traffic on a particular highway, as reported by ref. [42]. Another factor could be the distinctly different distribution profiles of coarse particles (2.5 μm < dp < 10 μm) and PM2.5 (dp < 2.5 μm), which was demonstrated by ref. [43].
Our findings that Fe, Zn, Ca, and Al were the most abundant metals in PM2.5 while Ca, Fe, Al, and Mg were the most abundant metals in coarse PM were confirmed by the results presented by ref. [43]. The metal distribution patterns in PM2.5 and coarse PM were similar, but their magnitudes differed, with Cd, Cr, Cu, Mn, Ni, and Zn claiming a much larger portion in PM2.5.
Cd, Cr, Cu, NI, Pb, and Zn are among the most common metal contaminates derived from roadways [44], but we discovered that Al, Fe, K, and Na metals were predominant in water, dust, and snow from the test site. These finding can be attributed to anthropogenic factors such as the use of de-icing agents on roads during the winter, fertilizer applications, and the direction of the area’s prevailing wind.
Our experiments discovered that Al, Fe, K, and Na metals had high concentrations and high mobility rates in water, dust, and snow. Despite higher Ca and Mg metal levels, their presence was only detected in dust particles. The metals Ce, Co, Cr, Cu, Dy, Er, La, Li, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn in dust particles, which were mostly present in residual form, were mostly of natural origin in the studied samples, were not highly mobilized, and were present in low quantities, which aligned with the results presented in ref. [44].
A metal’s mobility in water, dust, and snow might be traced to its physical and chemical properties. Based on their studies, the authors of ref. [43,45] affirmed the assertion that transition metals Zn, Cd, and Cu were the most soluble and Cr, Fe, and Ni were the least soluble, highlighting the importance of bioavailability in understanding the impact of transition metals on particle toxicity. Ref. [46] discovered that 63–71% of heavy metals were associated with particles smaller than 250 μm. Additionally, the smaller particle size fraction had a higher metal content, low density, and high mobility in runoff, thus posing a higher risk to the stream network. Ref. [47] reported that most metals in snow exhibited increased concentrations with decreasing pH, which enhanced their mobility. The high levels of Al, Ba, Fe, K, and Na metals in snow may be attributed to the alkalinity of the test site and they were regarded as the most mobile metals in snow.
The resuspension, deposition, and absorption of metals in water, dust, and snow are mainly attributed to road traffic, mostly through the breakdown and resuspension of coarse asphalt particles into fine particles by vehicular movements. Most of these particles end up in the atmosphere and on the edges of roadways.
Our findings showed that the chemical and physical properties of Al, Ba, Fe, K, and Na metals in snow varied depending on environmental factors such as temperature, pressure, polarity, molecular size, and alkalinity, which confirmed the results of ref. [48]. As a result, these factors influenced metal mobility in water, dust, and snow.

4.2. A Remote Sensing Approach for Monitoring Metal Pollution

Remote sensing data can be used as a tool for metal monitoring [49,50]. However, the use of satellite data has serious limitations due to cloud influence and the spatial resolution of remote sensing data.
Several scientists used hyperspectral data for metal mapping and monitoring [51,52]. This technique only offers information at a certain point in the assessment process, making it impossible to establish a detailed image of the dispersion of dusty particulates along highways. Repetitive sampling over time, which is costly and labor-intensive, does not allow for the collection of pollution data at precise sites but over only over a specified region [53], which adds to its challenges. We propose to overcome these limitations using UAVs. We suggested using a simple camera, which was cheaper, but the quality of the results were the same or better when compared with the results of ref. [54,55]. This technique is generic and can detect the levels of various metals and their distribution in the environment, such as roadways. On this foundation, we obtained information for the entire terrain reflecting all of its spatial features, specifically the micro-relief, and snow accumulation irregularities, which may have a significant impact on the distribution of metals in snow. Ref. [56] demonstrated this approach and our results confirmed these findings.
Ref. [57] reported that Cd, Co, Cr, Cu, Fe, Hg, Mn, Mo, Ni, Pb, and Zn metals can be detected based on remote sensing data. We found that only Al, Ba, Fe, K, and Na metals could be detected in snow. This was possible by employing UAV data and establishing the association between the metal content and the pixels of the separated UAV image colors. This technique aligned the metals with their unique corresponding color images (pixels), based on their content and distribution level for detection.
Several studies, including ref. [58], have investigated the spatiotemporal interpolation of UAV data and created a prototype of a standalone interpolation tool that uses radial basis functions (RBF) and inverse distance weighting (IDW) interpolation in a continuous space-time domain. Ref. [59] also demonstrated the successful application of USV to evaluate interpolation methods for distribution maps in chlorophyll-a monitoring. Because the transfer of this model to other regions or plots was not possible in this study, we only used the UAV to interpolate field point measurements. The findings of ref. [60] also affirmed the use of UAV data in spatial interpolation methods for assessing air quality in open-cast mines in an efficient and safe manner.
This study created an effective model for detecting Al, Ba, Fe, K, and Na pollution in snow. Furthermore, we discovered high pollution at 30–190 m from the roadway using UAV data. This model is advantageous for quickly tracking down high-pollution areas. It subsequently allows investigation and mitigation work to be accomplished in less time and at lower cost than conventional methods [61].

5. Conclusions

This paper proposes a technique in which UAV-based data may be utilized to detect metals in dust in snow-covered polluted locations. To support our claim, we evaluated the relationship between various metals in water (melted snow), dust, and snow with various UAV parameters.
The roadway was shown to be a polluter since samples approximately 30 to 50 m from the road had the highest metal concentrations, which declined with distance. In the case of Al, Ca, Fe, K, Na, and Mg metals, the occurrence of high metal distribution east of the highway may be attributed to the predominant wind direction at the test location throughout the research period (Figure 2, Figure 3 and Figure 4).
Al, Ba, Fe, K, and Na were shown to be visible in snow-covered polluted locations due to dust dispersal. UAV-based data improved the capability of identifying total metals in a mixture of dust and snow. Nonetheless, dust deposits are the best sign of pollution in snow. This discovery supports the claim that UAV indicators may be used to monitor untouchable pollution from roadways.

Author Contributions

Investigation: G.A.B., I.Y.S. and Y.I.V., writing-original draft preparation, G.A.B., I.Y.S. and Y.I.V. All authors have read and agreed to the published version of the manuscript.

Funding

The research received funding from the Ministry of Science and Highest Education of Russia (agreement no. 075-15-2022-321).

Data Availability Statement

The datasets generated and/or analyzed during the study are available from the corresponding author upon request.

Acknowledgments

The authors wish to express their gratitude to V.V. Dokuchaev Soil Science Institute, Moscow, for assisting with sampling, preparation, and analysis of samples at their laboratory. Additionally, this paper is supported by the RUDN University Strategic Academic Leadership Program.

Conflicts of Interest

The authors declare no conflict of interest.

Appendix A

For ground control of the UAV, we used 5 points, for which coordinates were obtained based on GNSS (geodesic class equipment, approximately 2 cm error in coordinate assessment). The average error for coordinate assessment by UAV was +/− 10 cm.
Table A1. Heavy metal levels in water from snow samples (µg/m2).
Table A1. Heavy metal levels in water from snow samples (µg/m2).
Heavy MetalDistance from the Road (m) and Point Code
19017015013011090705030030507090110130150170190
9W8W7W6W5W4W3W2W1W 1E2E3E4E5E6E7E8E9E
Al5.96.25.96.66.25.899.25.3136 490.3414.989.982.631.416483.6116.547.4
B5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Ba5.9286.2445.9426.6086.2065.7586.8425.2626.8 34.905891.27365.1385.164.494.6864.525.2964.738
Ca14821267.531732.091100.231337.391203.421724.181360.232196.4 2686.578245.741685.261609.921012.51363.63935.64884.432803.091
Cd5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964738
Ce5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Co5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Cr5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Cu5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Dy5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Er5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Eu5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Fe59.2862.4459.4266.0862.0657.5868.4252.6268 482.406371.05851.3851.644.946.8645.252.9647.38
Gd5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964738
Ho5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
K334.932508.886843.764379.96887.458702.476478.94939.267503.2 2142.01710.4821073.84665.64374.915414.711316.4278.04246.376
La5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Li5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Lu5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Mg305.292290.346317.897257.712269.961299.416335.258373.602499.8 372.59570.46418.747322.5237.97304.59196.62204.796161.092
Mn5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Na207.48437.081782.6726.88837.811727.4957.881841.73060 3333.72333.71798.31806763.3937.2723.2926.8615.94
Nd5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Ni5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
P5.9286.2445.9426.6086.2065.7586.8425.2626.8 39.2251.8651.3851.644.946.8645.252.9647.38
Pb5.9286.2445.9426.6086.2065.7586.8425.2626.8 39.2251.8651.3851.644.946.8645.252.9647.38
Pr5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Sc5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Sm5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Sr5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Tb5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Tm5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Y5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Yb5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Zn77.06453.07430.304262.77693.095.758239.4736.8346.8 56.86933.7095.13830.9629.18525.304494.9231.7764.738
Table A2. Heavy metal levels in dust from snow samples (µg/m2).
Table A2. Heavy metal levels in dust from snow samples (µg/m2).
Heavy MetalDistance from the Road (m) and Point Code
19017015013011090705030030507090110130150170190
9W8W7W6W5W4W3W2W1W 1E2E3E4E5E6E7E8E9E
Al0.220.150.380.541.061.82.83.679.47 108.6353.2422.6818.486.7613.571.413.370.98
B000000.010.010.030.03 0.090.050.020.030.010.04000
Ba0.030.050.110.260.080.150.893.340.84 87.56.1214.371.092.080.750.150.240.1
Ca10.56112.594.356.367.6324.05 187.6873.2618.6522.5910.486.261.211.91.19
Cd000000000 000000000
Ce00000.010.010.020.020.03 0.40.220.10.070.020.0400.010
Co00000000.010.01 0.090.050.020.020.010.01000
Cr0.01000.010.010.020.030.040.06 0.250.150.10.060.030.030.010.010
Cu00.010.010.010.020.020.030.080.1 0.660.250.220.110.060.040.010.010.01
Dy000000000 0.030.010000000
Er000000000 0.030.010.010.0100000
Eu000000000 000000000
Fe0.790.51.122.042.824.987.212.5425.25 232.94110.2652.4243.4717.6817.882.954.892.37
Gd0000000.010.010.01 0.040.020.010.0100000
Ho000000000 000000000
K0.110.10.370.20.390.891.212.185.77 37.4215.226.866.262.063.070.420.720.28
La0000000.010.010.02 0.20.110.050.040.010.0200.010
Li000000000 0.130.070.030.020.010.02000
Lu000000000 0.0100000000
Mg0.180.150.250.310.21.21.812.45.1 68.830.5910.7910.234.173.550.571.030.48
Mn0000.010.010.050.110.080.22 2.781.540.530.40.160.350.030.090.02
Na0.030.050.20.140.130.350.741.963.97 22.936.044.941.611.190.690.130.170.08
Nd000000.010.010.010.02 0.190.10.050.030.010.0200.010
Ni0000.010.010.010.020.040.04 0.220.110.060.050.020.0200.010
P0.260.30.430.420.931.132.312.733.01 19.6110.54.993.941.791.170.320.430.36
Pb0.020000.010.040.020.030.03 0.140.060.050.080.030.02000
Pr000000000 0.030.010.010.0100000
Sc000000000 0.030.010.010.0100000
Sm000000000 0.030.010.010.0100000
Sr00000000.040.07 1.450.270.220.040.040.0200.010
Tb000000.010.010.020 0.0200000000
Tm000000000 000000000
Y000000000.01 0.10.060.020.020.010.01000
Yb000000000 000000000
Zn0.030.020.030.050.030.070.140.240.024 1.820.940.40.330.170.130.020.030.02
Table A3. Heavy metal levels in snow samples (dust + water) (µg/m2).
Table A3. Heavy metal levels in snow samples (dust + water) (µg/m2).
Heavy MetalDistance from the Road (m) and Point Code
19017015013011090705030030507090110130150170190
9W8W7W6W5W4W3W2W1W 1E2E3E4E5E6E7E8E9E
Al6.126.356.287.147.267.61028.97145.47 598.93468.14112.58101.0838.16177.5785.01119.8748.38
B5.9286.2445.9426.6086.2065.7686.8525.2926.83 4.0125.2365.1585.194.54.7264.525.2964.738
Ba5.9586.2946.0526.8686.2865.9087.7328.6027.64 122.40697.393619.5086.256.575.4364.675.5364.838
Ca14831268.091733.091101.231339.981207.771730.541367.862220.45 2874.2583191703.911632.511022.981369.89936.85886.332804.281
Cd5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964738
Ce5.9286.2445.9426.6086.2165.7686.8625.2826.83 4.3225.4065.2385.234.514.7264.525.3064.738
Co5.9286.2445.9426.6086.2065.7586.8425.2726.81 4.0125.2365.1585.184.54.6964.525.2964.738
Cr5.9386.2445.9426.6186.2165.7786.8725.3026.86 4.1725.3365.2385.224.524.7164.535.3064.738
Cu5.9286.2545.9526.6186.2265.7786.8725.3426.9 4.5825.4365.3585.274.554.7264.535.3064.748
Dy5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9525.1965.1385.164.494.6864.525.2964.738
Er5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9525.1965.1485.174.494.6864.525.2964.738
Eu5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Fe60.0762.9460.5468.1264.8862.5675.6265.1693.25 715.346481.318103.895.0762.5864.7448.1557.8549.75
Gd5.9286.2445.9426.6086.2065.7586.8525.2726.81 3.9625.2065.1485.174.494.6864.525.2964738
Ho5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
K335.042508.986844.134380.16887.848703.366480.15941.447508.97 2179.43725.7021080.7671.9376.975417.781316.82278.76246.656
La5.9286.2445.9426.6086.2065.7586.8525.2726.82 4.1225.2965.1885.24.54.7064.525.3064.738
Li5.9286.2445.9426.6086.2065.7586.8425.2626.8 4.0525.2565.1685.184.54.7064.525.2964.738
Lu5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9325.1865.1385.164.494.6864.525.2964.738
Mg305.472290.496318.147258.022270.161300.616337.068376.002504.9 441.39601.05429.537332.73242.14308.14197.19205.826161.572
Mn5.9286.2445.9426.6186.2165.8086.9525.3427.02 6.7026.7265.6685.564.655.0364.555.3864.758
Na207.51437.131782.8727.02837.941727.75958.621843.663063.97 3356.632339.741803.241807.61764.49937.89723.33926.97616.02
Nd5.9286.2445.9426.6086.2065.7686.8525.2726.82 4.1125.2865.1885.194.54.7064.525.3064.738
Ni5.9286.2445.9426.6186.2165.7686.8625.3026.84 4.1425.2965.1985.214.514.7064.525.3064.738
P6.1886.5446.3727.0287.1366.8889.1527.9929.81 58.8362.3656.3755.5446.6948.0345.5253.3947.74
Pb5.9486.2445.9426.6086.2165.7986.8625.2926.83 39.3651.9251.4351.6844.9346.8845.252.9647.38
Pr5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9525.1965.1485.174.494.6864.525.2964.738
Sc5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9525.1965.1485.174.494.6864.525.2964.738
Sm5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9525.1965.1485.174.494.6864.525.2964.738
Sr5.9286.2445.9426.6086.2065.7586.8425.3026.87 5.3725.4565.3585.24.534.7064.525.3064.738
Tb5.9286.2445.9426.6086.2065.7686.8525.2826.8 3.9425.1865.1385.164.494.6864.525.2964.738
Tm5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Y5.9286.2445.9426.6086.2065.7586.8425.2626.81 4.0225.2465.1585.184.54.6964.525.2964.738
Yb5.9286.2445.9426.6086.2065.7586.8425.2626.8 3.9225.1865.1385.164.494.6864.525.2964.738
Zn77.09453.09430.334262.82693.125.828239.6137.0746.824 58.68934.6495.53831.2929.35525.434494.9431.8064.758
Table A4. UAV/remote sensing parameters of snow cover.
Table A4. UAV/remote sensing parameters of snow cover.
UAV ParametersParameters from the Road (m) and Point Code
19017015013011090705030030507090110130150170190
9W8W7W6W5W4W3W2W1W 1E2E3E4E5E6E7E8E9E
Blue_av128124124123121125125134141 154144131128123124124122123
Cyan135135136138141137137127119 106115128131135135135141139
Gray123122120119117121121131138 150141128125121121121117119
Green123122120119117121122131138 150141127124121121121118119
Hue147139156151146144140142150 157152157161145153155141145
Intensity116115114113111115115124130 142133121118114115114111112
Magnet132133135136138134133124117 105114128131134134134137136
Red120120119117114118118128136 149140127124120120120114116
Saturation634666654 544434366
Yellow127131131132134130130121114 101111124127132131131133132

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Figure 1. The location of the study area (54°36′15″ North, 38°6′20″ East) and collected samples in sealed buckets.
Figure 1. The location of the study area (54°36′15″ North, 38°6′20″ East) and collected samples in sealed buckets.
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Figure 2. Workflow of metal pollution detection based on UAV data.
Figure 2. Workflow of metal pollution detection based on UAV data.
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Figure 3. Distribution map of levels of (Al, Fe, K, and Na) metals in water.
Figure 3. Distribution map of levels of (Al, Fe, K, and Na) metals in water.
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Figure 4. Distribution map of levels of (Al, Ca, Ce, Co, Cr, Cu, Dy, Er, Fe, K, La, Li, Mg, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn) metals in dust.
Figure 4. Distribution map of levels of (Al, Ca, Ce, Co, Cr, Cu, Dy, Er, Fe, K, La, Li, Mg, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn) metals in dust.
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Figure 5. Distribution map of levels of (Al, Ba, Fe, K, and Na) metals in snow.
Figure 5. Distribution map of levels of (Al, Ba, Fe, K, and Na) metals in snow.
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Table 1. UAV color images.
Table 1. UAV color images.
Yellow=255 − Blue
Magenta=255 − green
Cyan=255 − red
Hue=Red − ((Green + Blue)/2) * 240/255
Saturation=√(Red2 + Green2 + Blue2 − Red * Green − Red * Blue − Green * Blue) * 240/255
Intensity=1/3 * (Red + Green + Blue) * 240/255
Gray=0.3 * Red + 0.59 * Green + 0.11 * Blue
Table 2. Correlation matrix between (Al, Fe, K, and Na) metals and UAV parameters.
Table 2. Correlation matrix between (Al, Fe, K, and Na) metals and UAV parameters.
MetalBlue_avCyanGrayGreenHueIntensityMagentaRedSaturationYellow
Al/m20.83−0.830.820.830.380.82−0.830.83−0.13−0.83
Fe/m20.84−0.830.830.840.300.84−0.840.83−0.02−0.84
K/m20.62−0.620.620.610.390.64−0.610.62−0.03−0.62
Na/m20.85−0.850.850.840.460.86−0.850.85−0.15−0.85
Table 3. Regression estimates of (Al, Fe, K, and Na) metals and UAV parameters.
Table 3. Regression estimates of (Al, Fe, K, and Na) metals and UAV parameters.
MetalParameterCoefficientsp-ValueFormula
Al/m2Red140.688 **0.0470.0567x + 117.67
Fe/m2Red161.131 **0.0160.0647x + 117.05
K/m2Intensity539.604 ***0.0060.0171x + 107.99
Na/m2Intensity744.159 *0.0690.0083x + 107.11
Multiple R0.936
R Square0.876
***, **, and * indicate 1%, 5%, and 10% levels of significance, respectively.
Table 4. Correlation matrix between (Al, Ca, Ce, Co, Cr, Cu, Dy, Er, Fe, K, La, Li, Mg, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn) metals and UAV parameters.
Table 4. Correlation matrix between (Al, Ca, Ce, Co, Cr, Cu, Dy, Er, Fe, K, La, Li, Mg, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn) metals and UAV parameters.
MetalBlue_avCyanGrayGreenHueIntensityMagentaRedSaturationYellow
Al/m20.86−0.860.850.850.450.86−0.850.86−0.10−0.86
Ca/m20.87−0.860.860.860.390.87−0.860.86−0.05−0.87
Ce/m20.86−0.860.850.850.450.86−0.850.86−0.09−0.86
Co/m20.88−0.890.880.870.460.88−0.870.89−0.14−0.88
Cr/m20.91−0.910.910.900.460.91−0.900.92−0.12−0.91
Cu/m20.87−0.870.860.860.450.87−0.860.87−0.10−0.87
Dy/m20.81−0.790.790.800.330.80−0.800.790.00−0.81
Er/m20.78−0.790.770.760.540.78−0.760.79−0.08−0.78
Fe/m20.87−0.870.860.860.450.87−0.860.87−0.10−0.87
K/m20.88−0.870.870.870.440.87−0.870.88−0.09−0.88
La/m20.87−0.800.860.860.450.87−0.860.87−0.10−0.87
Li/m20.82−0.840.810.810.460.82−0.810.83−0.12−0.82
Mg/m20.86−0.850.850.850.420.85−0.850.85−0.07−0.86
Mn/m20.86−0.860.850.850.440.86−0.850.86−0.09−0.86
Nd/m20.87−0.870.860.860.430.87−0.860.87−0.08−0.87
Ni/m20.90−0.900.890.890.430.90−0.890.90−0.08−0.90
P/m20.89−0.890.880.880.410.89−0.890.89−0.08−0.89
Pr/m20.82−0.830.820.810.520.82−0.810.83−0.12−0.82
Sc/m20.82−0.830.820.810.520.83−0.810.83−0.12−0.82
Sm/m20.82−0.830.820.810.520.83−0.810.83−0.12−0.82
Y/m20.86−0.870.860.850.470.86−0.850.87−0.14−0.86
Zn/m20.89−0.890.880.880.430.89−0.880.89−0.09−0.89
Table 5. Regression estimates of (Al, Ca, Ce, Co, Cr, Cu, Dy, Er, Fe, K, La, Li, Mg, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn) metals and UAV parameters.
Table 5. Regression estimates of (Al, Ca, Ce, Co, Cr, Cu, Dy, Er, Fe, K, La, Li, Mg, Mn, Nd, Ni, P, Pr, Sc, Sm, Y, and Zn) metals and UAV parameters.
MetalParameterCoefficientsp-ValueFormula
Al/m2Red33.842 **0.0140.3029x + 119.14
Ca/m2Red46.509 **0.0520.1813x + 119.59
Ce/m2Red0.129 **0.01280.567x + 119.08
Co/m2Red0.027 **0.011366.22x + 118.86
Cr/m2Red0.063 **0.013135.44x + 117.26
Cu/m2Red0.165 **0.04552.174x + 118.55
Dy/m2Red0.008 **0.0591028x + 121.05
Er/m2Red0.008 *0.071980x + 120.07
Fe/m2Red68.578 **0.0170.1441x + 118.99
K/m2Red9.009 **0.0440.9246x + 119.04
La/m2Red0.063 ***0.011162.11x + 119.01
Li/m2Red0.051 ***0.005235.22x + 119.67
Mg/m2Red20.183 **0.0240.484x + 119.49
Mn/m2Red0.911 **0.01011.581x + 119.18
Nd/m2Red0.059 **0.010172.79x + 118.92
Ni/m2Red0.050 **0.032157.53x + 117.91
P/m2Red5.008 **0.0241.7508x + 118.01
Pr/m2Red0.011 **0.019933.94x + 119.7
Sc/m2Red0.011 ***0.019933.94x + 119.7
Sm/m2Red0.011 ***0.019933.94x + 119.7
Y/m2Red0.035 ***0.005315.73x + 119.3
Zn/m2Red0.506 **0.01418.833x + 118.3
Multiple R0.942
R Square0.888
***, **, and * indicate 1%, 5%, and 10% levels of significance, respectively.
Table 6. Correlation matrix between (Al, Ba, Fe, K, Na) metals and UAV parameters.
Table 6. Correlation matrix between (Al, Ba, Fe, K, Na) metals and UAV parameters.
Blue_avCyanGrayGreenHueIntensityMagentaRedSaturationYellow
Al/m20.84−0.840.830.840.400.84−0.840.84−0.12−0.84
Ba/m20.85−0.850.840.850.340.85−0.850.85−0.06−0.85
Fe/m20.86−0.860.850.860.360.86−0.860.86−0.05−0.87
K/m20.64−0.640.630.620.390.65−0.620.64−0.04−0.64
Na/m20.85−0.850.850.840.450.86−0.840.85−0.15−0.85
Table 7. Regression estimates of (Al, Ba, Fe, K, and Na) metals and UAV parameters.
Table 7. Regression estimates of (Al, Ba, Fe, K, and Na) metals and UAV parameters.
MetalParameterCoefficientsp-ValueFormula
Al/m2Red174.530 **0.0320.0488x + 117.78
Ba/m2Red48.310 ***0.0080.2384x + 118.91
Fe/m2Red229.709 **0.0110.046x+ 117.48
K/m2Intensity539.699 ***0.0060.017x + 107.92
Na/m2Intensity744.855 *0.0690.0082x + 107.12
Multiple R0.941
R Square0.886
***, **, and * indicate 1%, 5%, and 10% levels of significance, respectively.
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Baah, G.A.; Savin, I.Y.; Vernyuk, Y.I. Pollution from Highways Detection Using Winter UAV Data. Drones 2023, 7, 178. https://doi.org/10.3390/drones7030178

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Baah GA, Savin IY, Vernyuk YI. Pollution from Highways Detection Using Winter UAV Data. Drones. 2023; 7(3):178. https://doi.org/10.3390/drones7030178

Chicago/Turabian Style

Baah, Gabriel A., Igor Yu. Savin, and Yuri I. Vernyuk. 2023. "Pollution from Highways Detection Using Winter UAV Data" Drones 7, no. 3: 178. https://doi.org/10.3390/drones7030178

APA Style

Baah, G. A., Savin, I. Y., & Vernyuk, Y. I. (2023). Pollution from Highways Detection Using Winter UAV Data. Drones, 7(3), 178. https://doi.org/10.3390/drones7030178

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