Dissolved and Suspended Forms of Metals and Metalloids in Snow Cover of Megacity: Partitioning and Deposition Rates in Western Moscow

: Concentrations and ratio of dissolved and suspended forms of metals and metalloids (MMs) in snow cover and their deposition rates from the atmosphere in the western part of Moscow were studied. Forms of MMs were separated using a ﬁlter with pore diameter of 0.45 µ m; their concentrations were measured by ICP-MS and ICP-AES methods. Anthropogenic impact in Moscow caused a signiﬁcant increase in dust load (2–7 times), concentration of solid particles in snow cover (2–5 times), and mineralization of snow meltwater (5–18 times) compared to the background level. Urban snow contains Sn, Ti, Bi, Al, W, Fe, Pb, V, Cr, Rb, Mo, Mn, As, Co, Cu, Ba, Sb, Mg mainly in suspended form, and Ca and Na in dissolved form. The role of suspended MMs in the city signiﬁcantly increases compared to the background region due to high dust load, usage of de-icing salts, and the change of acidic background conditions to alkaline ones. Anthropogenic emissions are the main sources of suspended Ca, W, Co, V, Sr, Ti, Mg, Na, Mo, Zn, Fe, Sb, and Cu in the snow cover of tra ﬃ c zone. These elements’ concentrations in roadside snow cover exceed the background values more than 25 times. The highest concentrations and deposition rates of MMs in the snow of Moscow are localized near the large and medium roads.


Introduction
Urban air pollution with particulate matter is a recognized environmental problem, especially relevant for megacities. Contaminated air is responsible for about 80% of premature deaths; it causes ischaemic heart disease, stroke, chronic obstructive pulmonary disease, and lung cancer [1], and increases the risk of adenocarcinomas [2]. Increased concentrations of particulate matter with high proportions of metals and metalloids (MMs) affect the external respiratory function of citizens, especially of asthma patients [3].
Due to its long occurrence and ability to accumulate pollutants over the entire cold period of the year, snow cover is a natural, informative, and convenient component indicating air pollution with particulate matter and MMs in northern cities [4][5][6][7]. Snow pollution with MMs correlates well with the overall Air Quality Index (AQI) and the level of atmospheric pollution with PM 10 and PM 2.5 [8]. In comparison to rains, snow more effectively absorbs pollutants and washes them out of the atmosphere due to the higher surface area and porosity of snowflakes compared to raindrops [9]. The intensity of snow cover pollution is determined from the mass of MMs entering soils and surface waters during snow melting. MMs in liquid (dissolved or soluble) form could be included into the biogeochemical cycle, while solid (suspended or insoluble) forms of MMs accumulate in surface Geochemical survey of snow cover was carried out in mid-March 2018 in maximum snow cover thickness. Due to frequent thawing weather in winter of 2017-2018, permanent snow cover was formed only at the end of the first decade of January 2018. The thickness of snow cover in WAO differed only slightly from the long-term mean values (35-45 cm) [51,54] and averaged 42-50 cm near roads, increasing to 55-65 cm (averaged 61 cm) within the background areas. It is known that MMs concentrations in the surface layer of snow cover are usually lower than in the underlying layers [12]. To avoid underestimation of snow cover pollution, snow samples were taken along the full depth of undisturbed snow cover. In total, 26 mixed samples were taken within the territory of WAO (Figure 1), each consisting of 10-15 individual samples taken at a distance of 3-5 m by plastic pipe with the cross-section area of 20 cm 2 (one plastic pipe corresponded to one snow core, i.e., snow column) along the following roads: the MRR (3 sites), highways with four lanes in one direction (4 sites), large roads with three lanes in one direction (4 sites), medium roads with two lanes in one direction (5 sites), and small roads with one lane in one direction (5 sites). The yards of residential Geochemical survey of snow cover was carried out in mid-March 2018 in maximum snow cover thickness. Due to frequent thawing weather in winter of 2017-2018, permanent snow cover was formed only at the end of the first decade of January 2018. The thickness of snow cover in WAO differed only slightly from the long-term mean values (35-45 cm) [51,54] and averaged 42-50 cm near roads, increasing to 55-65 cm (averaged 61 cm) within the background areas. It is known that MMs concentrations in the surface layer of snow cover are usually lower than in the underlying layers [12]. To avoid underestimation of snow cover pollution, snow samples were taken along the full depth of undisturbed snow cover. In total, 26 mixed samples were taken within the territory of WAO (Figure 1), each consisting of 10-15 individual samples taken at a distance of 3-5 m by plastic pipe with the cross-section area of 20 cm 2 (one plastic pipe corresponded to one snow core, i.e., snow column) along the following roads: the MRR (3 sites), highways with four lanes in one direction (4 sites), Atmosphere 2020, 11, 907 4 of 32 large roads with three lanes in one direction (4 sites), medium roads with two lanes in one direction (5 sites), and small roads with one lane in one direction (5 sites). The yards of residential buildings with car parking lots (four sites) and the Meteorological Observatory of the Lomonosov Moscow State University (MO MSU) were also sampled. The background area was chosen to be sufficiently distant from the city to avoid its polluting influence. Thus, three sampling sites were selected more than 120 km west of Moscow in the Mozhaisk and Volokolamsk districts of the Moscow Oblast.

Laboratory Analysis and Data Processing
Snow cover samples were melted in the laboratory at 20-22 • C. The main physicochemical characteristics of meltwater were determined at the Ecological and Geochemical Center of the Lomonosov Moscow State University, Faculty of Geography. The pH of the resulting solution was measured using the potentiometric method with the рНMeter "SevenCompact S220" (Mettler Toledo, Greifensee, Switzerland; accuracy: ±0.002). Filtration through membrane filters with pore diameter of 0.45 µm (EMD Millipore, Burlington, MA, USA) was applied to isolate filtrate with dissolved (or soluble) forms of MMs and particles on the filter with suspended (or insoluble) forms. Filters with pore diameter of 0.45 µm are widely used to separate the dissolved and suspended forms of MMs when studying the composition of snow cover, rainfall runoff, or river waters [8,16,55,56].
The anionic composition of filtrate (SO 4 2− , Cl -, NO 3 − ) was determined using the "Stayer" liquid ion chromatograph (Akvilon, Moscow, Russia); and the cationic composition (Ca 2+ , Mg 2+ , K + , Na + ) using the atomic absorption spectrometer with flame atomization "novAA-400" (Analytik-Jena AG, Jena, Germany). The detection limits for cations and anions were calculated at 95% confidence level for three parallel measurements of the sample and blank measurements. For SO 4 2− and Na + , they are 0.04 mg/L, for Ca 2+ and K + − 0.03 mg/L, for Cl -, NO 3 -, and Mg 2+ − 0.02 mg/L. The concentration of HCO 3 − ions was calculated as the difference between the sums of cations and anions equivalents. In aerosol chemistry, the ammonium plays a significant role in chemical processes, including the formation of secondary ammonium sulfate and ammonium nitrate fine inorganic aerosols [57]. However, previous studies on the chemical composition of snow in Moscow showed that the ammonium in urban snow is about 5%-eq. from the amount of cations [58]. That is, the ammonium does not play a significant role in the balance of cations in Moscow snow meltwater. Therefore, the concentrations of ammonium in snow cover of WAO were not measured. The content of solid particles in snow meltwater (X, mg/L) was estimated (Equation (1)) based on the mass of suspension on the filter m (mg), weighed on an analytical balance "Discovery DV114C" (Ohaus, Greifensee, Switzerland; repeatability: 0.1 mg): where V is the amount of meltwater (L). Concentrations of dissolved and suspended forms of Al, As, Ba, Bi, Ca, Cd, Co, Cr, Cu, Fe, K, Mg, Mn, Mo, Na, Ni, Pb, Rb, Sb, Sn, Sr, Ti, V, W, and Zn were measured at the laboratory of the N.M. Fedorovsky All-Russian Research Institute of Mineral Raw Materials (VIMS) by ICP-MS and ICP-AES methods using the "iCAP Qc" mass spectrometer (Thermo Fisher Scientific, Waltham, MA, USA) and the "Optima-4300DV" atomic emission spectrometer (Perkin Elmer, Waltham, MA, USA) according to the certified methods [59,60]. The VIMS laboratory is accredited to the Analytics international accreditation system (AAS.A.00255) and the national accreditation system (RA.RU.21ΓΠ11); it meets the requirements of the International Standards ISO Guide 34:2009, ISO/IEC 17025:2017, and ISO/IEC 17043:2010. The VIMS laboratory is also accredited to certificate measurement techniques and provide metrological examination in Russian Federation (accreditation certificate No. 01.00115-2013). The analysis was conducted using replicates, method blanks, field blanks, and standard reference materials in order to maintain the standard quality. For dissolved MMs, the detection limit (DL),which is defined as three times the standard deviation of replicate blank measurements, were as Snow cover contamination with dissolved and suspended forms of MMs was evaluated (Equation (2)) using the contamination factor (CF): where Curb and Cb are MMs concentrations in snow cover in the city and in the background area, respectively (µg/L). The mass of each MMs coming to the Earth's surface from the atmosphere (µg/m 2 per day), that is, the deposition rates of suspended and dissolved MMs were calculated (Equations (3) and (4)): where Durb and Db are deposition rates in the city and in the background area, respectively (µg/m 2 per day); P is the water supply in snow cover (L/m 2 ); t is the number of days of snow cover occurrence (61-63 days depending on the date of snow sampling). Water supply in snow cover was calculated according to Equation (5) below: where a is the number of plastic pipes with snow (i.e., snow columns or snow cores) collected at the site; S is the area of the plastic pipe cross-section, m 2 . The dust deposition rate was estimated as (Equation (6)): The intensity of anthropogenic pressure was determined (Equation (7)) as the excess of an element deposition rate on the studied urban area over its deposition rate on the background area: Comprehensive assessment of snow cover pollution with dissolved and suspended MMs was obtained by calculating the total contamination factor of snow (TCF, Equation (8)) and the total excess of MMs deposition rates in the city above the background (TDF, Equation (9)): where n is the number of chemical elements with CF or DF > 1; when calculating TCF and TDF, only CF and DF > 1 are summed [61,62]. The environmental hazard of MMs snow pollution was determined in line with the TCF gradations adopted in Russia: <32-low, Tulsa, OK, USA) with a measure of similarity d = 1-Person r and amalgamation rule Complete Linkage. The significance of Pearson correlation coefficients r and Spearman correlation coefficients r s was checked against the t-criterion at p < 0.05.

Physicochemical Properties and Macrocomposition of Snow Meltwater
Background snow waters in the western part of Moscow are slightly acidic (pH 5.6), with low mineralization (6.4 mg/L); the ionic composition of water is calcium bicarbonate ( Table 1). The obtained data correlates with the findings of physicochemical properties of snow in Moscow suburbs [40,58,63]. The concentration of solid particles in snow water in background conditions is low (about 9 mg/L), while the intensity of daily dust load (9 mg/m 2 per day) corresponds to the average level for background non-urbanized areas in the East European Plain (about 10 mg/m 2 per day) [61]. Table 1. Physicochemical properties, snow cover thickness, and ion content in snow meltwater in the western part of Moscow and the background territory.  pH value is an integral indicator of acidifying and alkalizing compounds' ratio and reflects the influence of these compounds on the carbonatic equilibrium. According to 2018 data, the pH value of contaminated snow meltwater in WAO ranged from 7.3 to 8.8 with an average of 8.1; that is, the alkalization of snow cover in the city is intensive and exceeds the background by 2.5 pH units. The highest pH values 7.6-8.8 are common for roads; with an average pH of 8.2, the alkalization of meltwater decreases in the following sequence of roads: large (8.6) > highways (8.4) > medium (8.2) > small and the MRR (8.0). The rising pH value of snow meltwater with an increase in traffic intensity was also recorded in Lahti, Finland [55]. The intensity of alkalization in WAO is lower in the yards of residential buildings with car parking lots-the average pH of snow meltwater is 7.4 with slight variations from 7.3 to 7.5. The pH of snow water in the territory of the MO MSU is 7.3, which is close to the mean value for residential zones. In Moscow, like most other cities, there is alkalinization of surface soil horizons [29,30,[64][65][66], road dust particles [65,67,68], and bottom sediments of lakes and ponds [69]. Previous studies on Moscow soil water extract and the composition of salts in soils showed a significant increase in the amount of carbonates [29], as opposed to the background sod-podzolic soils that do not contain carbonates at all. This, together with results of research in other cities [70], indicates significant influence of carbonates on the soils' pH value. The sources of carbonaceous compounds in the urban environments, aside from natural-originated carbonate particles, are dust from construction and demolition activities, as well as road dust particles mainly related to tire wear, motor exhaust, and brake wear [71][72][73]. Thus, rather high pH values of snow meltwater are associated with partial dissolution of incoming urban soils and road dust particles on snow cover surface. It is known that partial dissolution of solid particles of various geneses increase the rainwater pH values [74]. Greater pH values of roadside snow meltwater sampled near large roads confirm the hypothesis of road dust particles being the most important alkalizing agent for the snow of WAO. The pH of road dust water extract for Moscow large roads varies from 6.9 to 8.1 and decreases in the yards [68]. An additional source of alkalizing agents in snow cover is marble chips, which is a commonly used DIS in Moscow [75]. On the contrary, chloride DISs can slightly reduce the pH of precipitation and snow due to the formation of gaseous HCl, ClNO 2 , and Cl 2 as a result of the reaction of NaCl with gaseous HNO 3 , H 2 SO 4 , N 2 O 5 , and ClONO 2 [76].
The intensive geochemical impact of transport and industrial facilities and the application of DISs led to a significant increase in the concentration of solid particles in snow cover (2-5-fold), the intensity of dust load (2-7-fold), and mineralization (5-18-fold), as well as to the change in the ionic composition of snow meltwater in WAO relative to the background. The mineralization of meltwater next to roads in the western part of Moscow averages 100 mg/L, varying from 18 to 331 mg/L; in the yards of residential buildings, it varies from 18 to 63 mg/L and amounts 32 mg/L in the territory of the MO MSU. In terms of the mineralization of snow meltwater, the roads of WAO form a following series: highways (233 mg/L) > MRR (144) > large (87) > medium (73) > small (58 mg/L). In Moscow, the average annual concentrations of atmospheric PM 10 in 2018 totaled 0.7 of the maximum permissible concentrations (that is, about 40 µg/m 3 ); near highways, the concentration of PM 10 was 1.4 times higher than inside residential areas [35]. At the same time, PM 10 concentrations in the city decreased by an average of 3.7% annually in 2005-2014 [77]. Our data on snow cover pollution show an increase in the content of solid particles by almost four times in snow meltwater near roads compared to the yards of residential buildings with car parking lots, which indicates a significant contribution of particles larger than PM 10 to atmospheric deposition, as well as the presence of an additional source of solid particles in snow, e.g., DISs. A sharp increase in the content of particulate matter in snow cover when using DISs was also found in other cities, for example, in Yekaterinburg (Russia); where the content of particulate matter in the snow cover of roads and footpaths is 4-5 times higher than in the snow cover of lawns and car parking lots in the yards [21].
The ionic composition of snow meltwater near the Moscow Ring Road, the highways, and large and medium roads differs slightly. It is almost everywhere of calcium-sodium chloride type, which compares favorably with the results of long-term (1999-2019) studies of acidity and chemical composition of snow and rainfall in Moscow and Moscow Region [58,63,78]. Only at sampling points on the streets of Molodogvardeiskaya (point S16 in Figure 1) and Ryabinovaya (point S08) near the construction sites and industrial zones Severnoye Ochakovo and Yuzhnoye Ochakovo is the water of calcium-sodium bicarbonate-chloride type. Snow meltwater near small roads, at car parking lots in the yards of residential buildings, and on the territory of the MO MSU has the same composition with slightly higher proportion of bicarbonates, nitrates, sulfates, and calcium and lower proportion of chlorides and sodium, probably due to smaller amounts of DISs, which is also confirmed by low mineralization of meltwater on these territories as compared to other roads.
Water supply in the snow cover next to the roads is average 80 L/m 2 , slightly decreasing in the yards (79 L/m 2 ) and the MO MSU (77 L/m 2 ). Water supplies in the background snow cover are lower and amounts to 67 L/m 2 as a result of partial snow blowing by the wind. Snow cover in the city is less susceptible to blowing due to higher density resulting from slightly higher air temperatures (heat island) and, accordingly, more frequent temperature transitions around 0 • C in March (during snow cover sampling period) and the earlier start of snow melting.

Dissolved Forms of MMs
Average, minimum, and maximum concentrations of MMs forms in snow cover near roads, in the yards of residential buildings, near the MO MSU, and in the background area are given in Table 2. The value of contamination factor CF (Table 4) shows the excess of MMs forms' concentrations above the background level and, therefore, the level of snow cover contamination.
The maximum content of dissolved forms of most MMs is observed in roadside snow cover, because of vehicular impact; it gradually decreases in the yards and at the MO MSU down to minimum levels in snow cover of the background territory in the suburbs. The CF factor varies quite a lot along the roads with different traffic intensities in WAO. The snow cover is most heavily contaminated with dissolved Na, the CF of which regularly declines as the road size decreases: from 280 near the highways, 134 near the MRR and 50-70 near large, medium and small roads, and down to 28-31 in the yards of residential buildings and at the MO MSU. The main source of dissolved Na is DISs; thus, dissolved Ca and Sr actively accumulate in snow cover too. Their CFs also decline as the road size decreases: from 14-23 at the MRR and highways to 6-10 on large, medium, and small roads, and down to 3-6 in the yards and at the MO MSU. High values of correlation coefficient r for pairs Na-Cl − (0.99), Ca-Cl − (0.87), and Sr-Cl − (0.94) indicate the entry of these metals with chloride-type DISs, applied frequently in Moscow. This is confirmed by the studies of snow cover composition in the southwestern part of Moscow, where the use of DISs contributed to a sharp increase in Na, Ca, and K concentrations [39].
Motor vehicle emissions could be an additional source of Na. Petrol Euro 3, 4, 5 and diesel Euro 3, 4 vehicles emit up to 1310 µg Na per 1 km [80]. Strontium is probably an impurity in DISs, since this metal is often a part of calcium compounds. Concentrations of dissolved forms of MMs in snow cover depend on the intensity of transport impact; they are also associated with different amounts of DISs applied on different roads. For example, the concentrations of Na in snow of Novi Sad (Serbia), those of Cu, Fe, Zn, and Pb in snow of Beijing (China), and those of Al, Co, Cr, Cu, Mn, and Ni in snow of Lahti (Finland) increase with larger road size, while the concentrations of Zn in Novi Sad and Clin Beijing decrease [4,12,55].
In the western part of Moscow, several MMs showed local maxima of concentrations in the yards and at the MO MSU, where large areas are occupied by parking lots. Thus, high levels of dissolved K are probably due to the active fuel combustion during car engine idling; this is confirmed by the value of r = 0.57 between the content of dissolved K and NO 3 -. It is known that NO 3 is produced by fuel burning, in particular by motor transport [81], amounting up to 2280 µg NO 3 per 1 km [80].
Even larger amounts of water-soluble NO 3 are released when burning diesel fuel [82]. Therefore, K is used as an indicator of vehicle emissions when studying the composition of aerosols [83,84]. It occurs in unleaded gasoline [85] and comes abundantly with road dust, especially in tunnels, and with direct tailpipe emissions of cars [80,86,87]. Fuel burning also causes the release of V into the environment [88,89], and therefore its concentrations are high in the snow cover near parking lots.
In general, MMs emissions over cruise conditions are substantially different from the emissions over a transient cycle or while idling [90].  Notes. The CF value of each element is written in the subscript. DS-dissolved (blue background), SP-suspended (orange background) forms.
Atmosphere 2020, 11, 907 11 of 32 Besides the above-mentioned Na, Ca, Sr, K, and V due to the transport impact, the snow cover near all types of roads is highly polluted (CF > 3) with dissolved Mo and Mg, with W, Co, and Ba near the MRR, with W, Sn, Bi, Co, Ni, Ba, Sb, Fe, and Ti near highways, with Sb and Co near large roads, with Cd, Mn, and Co near medium roads, and with Sb, Ba, and Ni along small roads. The possible source of these MMs could be non-exhaust vehicle emissions [91][92][93][94], which is supported by the data on the intensive enrichment of Moscow road dust and especially its fractions PM 1 and PM 1-10 with Sb, W, Sn, Bi, and Cd [67,95,96], and nanoscale particles of road dust enriched with Pb, Cu, Zn, Ni, Cd, Cr, Co, and Sn [97]. Therefore, the highest CF values for many of these MMs, in particular W and Sn, are characteristic of snow cover along the MRR and highways. High levels of dissolved Na, K, Mg, Fe, Al, Zn, Sr, Cu, and other MMs comparable to our data were also found in snow cover near the MRR in 2011 [48].
The Mo and Sb in snow cover is also characteristic of the eastern part of Moscow, where these elements are actively emitted by heat and power stations, as well as by metalworking, mechanical engineering, and petrochemical enterprises [46]. The MO MSU and the background territory are characterized by higher concentrations of dissolved Zn and Pb compared to snow cover along the roads and in the yards. The increased content of dissolved Zn in snow cover near the MO MSU compared to roadside snow cover was indicated earlier [40]. This is probably due to the regional transfer of pollutants from urbanized areas of the Moscow Oblast and the nearest regions, to the macro-regional transfer from Europe and global migration of pollutants. It is confirmed by the data on the accumulation of metals in the dust component of background snow cover near Zvenigorod in the western part of Moscow Oblast [46], in snow cover of the background regions of the Ryazan Meshchera [98], and the Polar Plateau in Antarctica [99]. High levels of Cd at the urban reference sites not polluted by traffic compared to snow near the roads were detected in Innsbruck, due to the input of metal from non-transport sources [23]. In Moscow, the snow cover composition at the MO MSU showed 2-3 times higher content of Fe, V, Co, and Ba; minor difference in content of Al, Mn, Ni, Cu, As, and Cd; and 2-3 times lower content of Cr, Zn, Sr, and Mo compared to the territory of the Botanical Garden next to the MO MSU [40].
Different rates of CF value increment with increasing anthropogenic impact make it necessary to consider the behavior of all studied pollutants simultaneously and make an integral assessment of contamination. For this purpose, total contamination factor TCF of snow cover with dissolved and suspended MMs was calculated. The spatial distribution of TCF is shown in Figure 2.    Figure 1) roads. Territories along almost all studied small roads and at the MO MSU have the high level of pollution (with TCF 64-128) and a dangerous environmental situation. The amount of applied DISs is lower in most yards, and the impact of transport decreases as well, but it does not completely disappear because of the presence of car parking lots. The decrease is also due to protective functions of buildings that act as barriers to air pollutant flows from the highways to the yards of residential buildings [100]. Buildings prevent the spread of emissions from vehicles, thus decreasing snow cover pollution to medium level (with TCF 32-64) and a moderately dangerous environmental situation.

Suspended Forms of MMs
The content of suspended forms of all MMs in roadside snow cover is higher than in snow cover of the yards, the MO MSU, and the background territory. Application of DISs on roads and further blowing of their particles by the wind leads to their inclusion into roadside snow. This accounts for the fact that the highest CF values of Ca (385, 64, and 24, respectively) were found in snow cover of the MRR, highways, and large roads, decreasing on medium roads, small roads, in yards, and at the MO MSU (21, 13, 9, and 10, respectively). Suspended forms of all MMs, except K, Mo, and Sb, are accumulated much more intensively than dissolved ones, due to enrichment of the dust component of snow cover with MMs and the high content of solid particles in snow cover. Solid particles' input to the snow cover is due to precipitation from the atmosphere, DISs application on roads, blowing of road dust and soils particles from snow-free areas, and spraying of mud sediment from the surface of roadways during snow melting. Resuspended road dust is reported to be one of the most important sources of microparticles in the atmosphere; for example, in Bogota, it supplies about 23% of the mass of PM 10 particles [101] and in the USA, more than a half of PM 10 and about a quarter of PM 2.5 particles [102]. In Paris, the contributions of road dust emissions were estimated to be 13% of atmospheric PM 10 , while the sum of vehicle exhaust and wear accounted for 47% of PM 10 [103]. Moreover, for the north cities, the spraying of mud sediment from the surface of roadways is an essential source of suspended particles and MMs in roadside snow cover [21].
On large roads, dissolved Mo and Sb accumulate more intensively compared to its suspended forms, which is probably due to the increased pH of snow meltwater (an average of 8.6 on large roads, 8.0-8.4 on other roads). These elements are typical anionogenic elements and migrate well in alkaline conditions, so the higher pH values could contribute to the acceleration of their dissolution [104]. A positive correlation of dissolved Mo content with pH values of river water and snow was also found in the basins of rivers flowing into the Gulf of Bothnia [105].
Smaller roads have lower traffic intensity, resulting in a decrease of accumulation of suspended MMs forms. Ca, W, Co, Ti, Mg, Sr, Na, Mo, Al, Fe, Zn, Sb, Mn, As, Ba, Cu, Cr, Ni, Rb, Sn, and K are accumulated intensively (CF > 50) in snow cover near the MRR. The CF decreases sharply for all MMs along the highways, reaching 64 for Ca, 27-47 for W, Co, Ti, Sr, V, Mg, and Na and less than 25 for other MMs. Along large and medium roads, the CF of Ca, W, Cu, Mo, Zn, Sr, Co, Sn, Sb, Mg, V, Ti, As, Na, Cu, and Fe decrease to 10-25, and to 5-17 near small roads. Higher content of solid particles in snow cover at the MO MSU leads to the increase in CF values for Zn, Mo, Cr, Sr, V, Pb, and Ca up to 10-16, as compared with the yards where CF values of these MMs are 5-9. High levels of Zn at the MO MSU are probably due to the influence of transport, since car parking lots are located nearby, where intense accumulation of the metal is typical [106]. Our studies on the chemical composition of dust component in snow cover of the eastern industrial part of Moscow showed that the following MMs are the ones that accumulate most intensively (the CF value is written in subscript): Mo 19 Sb 4.9 As 4.6 W 4.3 Sn 3.6 V 2.1 Fe 2.1 Cr 2.0 [46]. However, foregoing data include areas with low levels of snow cover pollution, namely recreational and agricultural zones; therefore, CF levels for MMs are lower than those obtained for the traffic zone in the western part of the city.
The TCF values of suspended MMs increase considerably and the levels of environmental hazard increase by one gradation at many points, as compared to the total pollution of snow cover with dissolved forms. The highest increase of TCF for suspended forms is at the MRR, where the extremely dangerous environmental situation and the maximum TCF values were found, ranging from 761 in the northern part of the study area (4.5 times higher than the TCF for dissolved MMs forms) to 1296 on the average (6 times higher) and 7580 in the southern part (39 times higher). In other territories, the growth of TCF for suspended forms relative to the dissolved ones is less pronounced, reaching 1.2 to 3 times. The exception is Rublevskoye Highway, where the TCF is almost 6 times lower due to the low dust content in snow cover (12 mg/L compared to 102 mg/L near the MRR). The low dust content in snow cover could be attributed to the large distance of sampling point from the highway itself-there is both an alternate route and a car parking lot on the roadside, which separate the sampling point from the highway.
Extremely high snow cover pollution on the territory near the intersection of the MRR and Leninskiy Avenue, one of the busiest highways in Moscow, is probably the result of very intense MMs inflow with vehicle emissions (enormous numbers of cars and traffic congestions), as well as the blowing of contaminated road dust microparticles. An extremely dangerous situation (TCF > 256) also occurs on Kutuzovskiy Avenue, Mozhaiskoye and Aminievskoye highways, and a number of large (Minskaya and Mosfilmovskaya streets) and medium (Molodogvardeiskaya and Bolshaya Filevskaya streets-sites S16 and S12 in Figure 1, respectively) roads. In the yards of residential buildings, snow cover pollution with suspended forms of MMs as compared to dissolved ones increases to the high level (TCF 64-128), and to very high level (TCF 128-256), and very dangerous environmental situation for small and some medium roads.
Thus, snow cover pollution on the roadside territories in the western part of Moscow is mainly due to particulate matter. It is enriched with Ca, W, Co, V, Sr, Ti, Mg, Na, Mo, Zn, Fe, Sb, and Cu. The MMs content in suspension along the roads is on average 25 times or more above the background. Na, Sr, Ca, K, Mo, Sb, and W are the main dissolved pollutants; their content in the snow of certain areas of the WAO is six or more times above the background level. The spatial pattern of the total contamination factor TCF is characterized by the formation of common centers of abnormally high values for both dissolved and suspended MMs forms on the MRR, Kutuzovskiy Avenue, Rublevskoye, Mozhaiskoye, and Aminievskoye highways and some other streets. The anomalies appear due to the application of DISs, vehicle emissions, as well as the impact of enterprises in the adjacent industrial zones, such as Severnoye Ochakovo, Yuzhnoye Ochakovo, Kuntsevo, Fili, and Western Port.

Partitioning of MMs
Studying the ratio of MMs forms is important for predicting the pollutants' behavior during and after snowmelt, since the dissolved phase has a higher migratory ability. Therefore, the risk of contamination greatly depends on the MMs' ability to transform from a non-dissolved phase to a dissolved one. To define the predominant phase of elements in snow, the share of their dissolved phase, or solubility (Kz, %) was calculated: Kz = 100% · Cdis/(Cdis + Csus), where Cdis is the concentration of dissolved phase of MMs, µg/L; Csus is the concentration of suspended phase, µg/L.
Most MMs in snow cover of the background territory prevail in dissolved form: the proportion of dissolved forms of Ca, Zn, Na, Cd, Ni, As, Cu, and Sr is more than 85%; 60-70% for Sb, Co, Mg, Mn, and Ba, and 52-56% for Rb and Mo (Figure 3). These MMs are most likely washed out from the atmosphere and could enter the snow cover during in-cloud processes, i.e., elements' sorption on snowflakes inside the cloud [107]. Another source is washing out from the atmosphere with an ultrafine (<0.45 µm) fraction of aerosols, which passes through filters in the process of snow meltwater filtration in the laboratory. The predominance of dissolved forms of MMs could also be attributed to a slightly acidic reaction (pH 5.6) of snow meltwater in background areas, as the cationogenic Ca, Zn, Na, Cd, Ni, Cu, Sr, Co, Mg, and Ba could be easily transferred from insoluble to soluble form in acidic waters [104,108,109].
Other MMs are found predominately in suspended forms, which accounts for 80-90% of Sn and Bi, 60-80% of Ti, Al, Fe, and W, and 50-60% of Pb, V, Cr, and K. An increase in the proportion of suspended forms of MMs is related to the washout of the solid aerosol particles in the atmospheric surface layer by below-cloud scavenging processes [107]. In the background area, most of these MMs enter the atmosphere with relatively large soil particles blown from snow-free surfaces, thus contributing to higher proportion of suspended MMs forms. Thin snow cover, strong wind, and the absence of woody vegetation could significantly increase the soil particles supply to the roadside snow. Regional transport of contaminated atmospheric aerosol particles of different sizes also contributes to the higher proportion of suspended MMs forms. For example, in Northern China, Al and Fe in precipitation are mainly associated with large particles and Pb with thin ones, while K, V, and Cr have a bimodal distribution with peak concentrations within particle size intervals of 0.43-0.65 and 4.7-5.8 µm [110].
In urban areas, mass deposition of solid particles from the atmosphere and the application of DISs on roads with their subsequent blowing out and re-depositing on the surface of roadside snow cover significantly increase the role of suspended MMs forms. This is most pronounced in snow cover along roads (Figure 3), where the proportion of suspended forms is above 90% for Sn, Ti, Bi, Al, W, and Fe, 80-90% for Pb, V, and Cr, 50-80% for Rb, Mo, Mn, As, Co, Cu, Ba, Sb, Mg, and Zn. The dissolved phase prevails for K, Ni, Cd, and Sr (it accounts for 50-65%), as well as for Ca (87%) and Na (97%).
The effect of dust deposition on the increasing proportion of suspended forms of MMs is confirmed by the high significant negative coefficients of rank correlation r s between the dust load and the proportion of dissolved forms for almost all MMs: r s are less than −0.67 for all MMs, except K (−0.57), Sb (−0.56), Ni (−0.41), and insignificant for Mo, W, and Na. Insignificant correlation between Mo and W solubility and dust load is due to numerous points with concentrations below the detection limit, for these elements. Weak Na solubility correlation with amount of dust particles is due to Na input mainly with DISs and their subsequent rapid dissolution, providing for just little effect on the dust load. High positive r s between the concentrations of Cl − in meltwater and the proportion of suspended forms of all MMs (r s = 0.49-0.75), except Sr (0.44), Ca (0.40), K, Ni, Mo, W (0.15-0.34), and Na (−0.28) indicate the presence of MMs as slightly soluble impurities in chloride DISs. High proportion of suspended MMs in snow cover of the WAO could be also explained by the change of subacidic conditions in background snow meltwater (pH 5.6) to neutral, weak alkaline, and even alkaline in the city (pH 7.5-8.6). Under such alkaline conditions, the cationogens Bi, Fe, Pb, Rb, Mn, Co, Cu, Ba, Mg, and Zn are poorly dissolved from the suspended particles. This is confirmed by the negative significant r s between the pH value of meltwater and the proportion of dissolved forms of Cu, Cd, Ba, Bi, Fe, Sn, Al, and W.
A comparative analysis of the chemical composition of atmospheric dust, snowmelt-runoff, and rainfall-runoff in Beijing showed the leading role of dust in the formation of precipitation composition. Its presence in the snow cover results in the predominance of suspended forms of pollutants [12]. High proportions of many MMs in the suspension along with the dissolved forms of Na, K, Ca, Sr, and Sb were also identified in snow cover on the windward slope of the Salt Lake Valley (central Wasatch Mountains), Utah, USA [111]. The predominance of suspended forms of most MMs seems to be typical of urban areas, as supported by the data on Cr, Pb, Cu, Ni, Al, and Fe in snow in Östersund [15] and on Pb, Cu, Zn, and Cd in snow in Luleå and Umeå, Sweden [16]. Atmosphere 2020, 11, x FOR PEER REVIEW 15 of 31  Concentrations of Al, Fe, Mn, and V in snow cover of the traffic zone increase with increasing particle size reaching the maximum in particles >1000 µm, while the concentrations of Zn and Pb are the highest in particles < 100 µm [21]. This trend is observed even in small cities with no industrial enterprises, where the increasing contributions of 0.45-1.2 µm, 1.2-8 µm, and >8 µm fractions to the total concentrations of these MMs in snow cause lower proportion of dissolved forms of Al, Si, Mn, Fe, and Zn compared to the background territories, as shown by the Valday case study [112]. A summary of the results of studies on the chemical composition and the ratio of pollutants in water runoff from roads at 294 monitoring points on six continents showed that Pb and Cr predominate in road runoff in suspended form, while Zn, Cu, Ni, and Cd in dissolved form [14]. At the same time, the proportion of suspended forms of MMs in snow meltwater is usually greater than in rainwater [113].
The MRR stands out among all types of roads of the WAO in terms of the ratio of MMs forms in snow cover-the highest proportion of suspended forms of all MMs was recorded next to this highway. Mass input of dust particles leads to the dominance of suspended form for most MMs in snow cover (more than 85%); only Cd and Sr account for 72-77%. Ca and Na entering snow cover with easily soluble DISs prevail in dissolved forms (61% and 86%, respectively). Medium roads, similar to the MRR, are characterized by a significant proportion (>80%) of suspended forms for Sn, Ti, Bi, Al, W, Fe, Pb, V, Cr, and Mo and relatively low ones for Zn and Cd (43% and 31%, respectively). A high proportion of dissolved Zn reaching 70% is typical of traffic area runoff [14], and of dissolved Cd and Zn for snowmelt water, in which the solubility of these metals could reach 100% and 81%, respectively [15]. The ratio of MMs forms on large, small roads, and highways is scarcely different from the average level for all WAO roads.
Anthropogenic load in the yards and at the MO MSU is less pronounced compared to roads; it is evident from the content of solid particles in snow meltwater (15 and 17 mg/L compared to 48 mg/L on the roads). Therefore, the contribution of suspended MMs to the total content of elements in snow cover decreases. The MO MSU is located between two small roads-Academician Khokhlov Street and Michurinskiy Alley, used for the passage and parking of vehicles of the MSU employees. Thus, the ratio of suspended and dissolved MMs forms is close to that in the yards. At the same time, the share of dissolved Cd, K, Zn, Mg, Ba, Cu, and Rb increases by 10% and more in snow cover at the MO MSU and in the yards of residential buildings compared with roads. The source of these MMs could be fine particles (less than 0.45 µm) emitted during the heating of car engines at car parking lots in the yards and near the MO MSU. This is confirmed by laboratory studies on the influence of air temperatures and the operation modes of car engines on snow pollution with particulate matter and MMs. The studies have shown that motor vehicles emissions enrich snow with particles of 50-400 nm, which are high in MMs content [19]. Therefore, when a solid phase is separated from meltwater using filters with 0.45 µm pore diameter, a large number of fine MMs-contaminated particles enters the dissolved phase. Nanoparticles account for 71% of the total number of particles with 3 nm to 10 µm diameter in snow of Montreal, and up to 19% of particles are less than 100 nm [114]. Particle number density of ultrafine particles (0.01-0.1 µm in diameter) in snow is dozens and hundreds of times larger than that of 0.1-0.2 µm and 0.2-0.5 µm particles. However, a significant proportion of Al, Cr, Mn, Co, Ni, Cu, As, Cd, and Pb is in suspended form, that is, it is associated with particles larger than 0.2 µm, although the ultrafine fraction also plays an important role in the formation of total MMs content in snow [22].
Study of the composition of atmospheric particles in Hong Kong revealed that the proportion of water-soluble MMs in PM 2.5 fraction is 10-25% higher than in the PM 10 fraction. Moreover, Ca, Mg, Cd, Zn, V, Cu, Mn, and Ni prevail in dissolved form in PM 2.5 fraction, compared to just Ca, Mg, Cd, and Zn in PM 10 [84]. Residential buildings often form enclosed spaces, or "well traps," in which the migration of particles in the atmosphere diminishes sharply and soil pollution with MMs in the yards increases [100] due to deposition of fine particles, thus contributing to a higher proportion of dissolved forms of MMs in snow cover. Probably for the same reason, the proportion of dissolved forms of most MMs (except Ni, K, and Mg) in snow cover of the yards is higher than at the MO MSU.
The traffic intensity at car parking lots is low-even near stores, the vehicles' turnover usually does not exceed 50 units per day per 1 parking place [115]; nevertheless, the runoff from these areas is usually highly enriched with many MMs as compared to highways with light traffic intensity [14].
Thus, Sn, Ti, Bi, Al, W, Fe, Pb, V, Cr, Rb, Mo, Mn, As, Co, Cu, Ba, Sb, and Mg dominate in suspended form in snow cover in the western part of Moscow. Ca and Na prevail in the dissolved form, and the contribution of suspended and dissolved forms of Zn, K, Ni, Cd, and Sr to their total content ranges from 40 to 60%, that is, they lack a clearly pronounced predominant form of occurrence.

Deposition Rates of Dissolved and Suspended MMs
To assess geochemical impact on the components of urban landscapes during the snow occurrence period, it is necessary to determine the accumulated supplies of MMs released during snow melting. The content of particulate matter and MMs in snow meltwater of urban areas is greater than in rainfall-runoff, indicating the crucial role of snow melting for the formation of chemical composition of river runoff [12,15]. Snow-covered areas near different types of roads, in the yards, and in the background territory are quite different, because the city territory is severely fragmented by the road network and buildings. Therefore, the correct comparison of the supplies of pollutants in snow cover of different territories is only possible using specific parameters (per unit area). Normalizing of supplies by the number of days of snow occurrence shows the accumulation of pollutants per unit area and per time unit, i.e., the daily intensity of deposition (flux) of pollutants from the atmosphere. Since the concentrations of dissolved and suspended forms of MMs are expressed in µg/L, data on water content in snow cover in L/m 2 are used to estimate the intensity of pollutants deposition.
The mean, minimum, and maximum values of the dissolved and suspended forms of MMs deposition from the atmosphere near the roads, in the yards of WAO, at the MO MSU, and in the background area are given in Table 5.
High levels of daily deposition in dissolved form are typical for major elements in precipitation, namely Na, Ca, K, and Mg; elements of the upper continental crust, i.e., Al and Fe, as well as Ti, are added to them if we consider the deposition in suspended form. Deposition of dissolved Na, Ca, Sr, Mo, K, W, Sb, V (DF > 5) and suspended Ca, W, Co, V, Ti, Sr, Mg, Na, Mo, Zn, Fe, Sb, Al, Cu, As, Sn, Ba (DF > 25) in roadside snow cover showed the largest excess above the background values. The list of priority pollutants is shorter at car parking lots in the yards of residential buildings of the Moscow WAO and the MO MSU. In the yards compared to the background areas, the highest excess of deposition rates are found for dissolved Na, K, and Sr (DF > 5) and suspended Ca, Sn, and Mo (DF > 10), while dissolved Na, K, Sr, and V and suspended Zn, Mo, Cr, Sr, V, Pb, Cu, Ca, As, Sn, and Sb are characterized by the highest excess of deposition rates at the MO MSU, compared to the background areas. Thus, the snow cover composition and MMs deposition intensity for the MO MSU territory showed intermediate values between yards and roads. This is mainly due to the amount and composition of deposited dust within MO MSU, since the distribution pattern of the dissolved forms is practically similar to the yards.
The total excess of MMs deposition rates over the background level is represented by the integral TDF index. For the dissolved MMs phase, the TDF value depends on the size of the road: it is maximum for the highways (446), on the MRR it is 264; it decreases to 186 on large roads, to 143 on medium roads and to 116 on small ones (Figure 4). Table 4. Mean, minimum, and maximum daily deposition rates of dissolved and suspended forms of MMs near roads, at car parking lots in the yards of residential buildings, near the MO MSU, and in the background area in March 2018, µg/m 2 per day.  composition of deposited dust within MO MSU, since the distribution pattern of the dissolved forms is practically similar to the yards. The total excess of MMs deposition rates over the background level is represented by the integral TDF index. For the dissolved MMs phase, the TDF value depends on the size of the road: it is maximum for the highways (446), on the MRR it is 264; it decreases to 186 on large roads, to 143 on medium roads and to 116 on small ones (Figure 4).  High TDF values are marked for Kutuzovskiy Avenue and Mozhaiskoye highway-648 and 529, respectively ( Figure 5). Increased values of the integral index (TDF > 250) were also calculated for the MRR, Rublevskoye, and Aminievskoye highways and Minskaya Street (a large road). TDF values are approximately the same in the yards and at the MO MSU (82 and 83, respectively). In addition, the changes in TDF values are determined by the accumulation of Na: the share of this metal to TDF is 67-68% for the MRR and the highways, decreasing to 59% for medium roads due to the less intensive use of DISs, to 51% for small roads, 45% in the yards, and 38% at the MO MSU. However, the contribution of Na is only 38% for large roads, because of the intensive input of dissolved forms of Mo and Sb (DF 40 and 19, respectively). A significant contribution of Ca, Sr, and K is common to all types of roads.

MMs
The maximum value of the integral TDF index for suspended phase, reaching 4039, is found for the MRR, due to intense deposition of a wide range The TDF value for suspended MMs within the MO MSU area lies between values for small roads and yards and equals to 189. There is no particular element leading in its contribution to TDF in suspended phase compared with dissolved one: the input of Zn averages 10%, those of Ca, V, Cr, Cu, As, Sr, Mo, Sn, Sb, and Pb-6-8%, and 5% or less of other MMs. On the roads, the contribution of Ca is 7-13%, W-7-10%, Mo and Cu-below 9%, Co and V-below 8%, Sn and Ti-below 7%, Sb, Zn, Sr, Mg, and Na-below 6%, and the rest MMs-5% or less. In the yards, the contribution of Ca is 9%, Mo, Sn, Sb, W, V, Zn, As, Ti, and Sr-6-8%, and the rest MMs-5% or less.     [46]. However, the calculation of TDF in the Eastern Okrug did not consider major elements that play an important role in snow cover pollution, such as Ca, Mg, Na, K, and Al, as well as Ba and Rb. If these elements are ignored, the TDF for the Western Okrug will be 574, which is very close to its value in the eastern industrial part of Moscow.

Indication of Sources (Cluster Analysis)
Sources of dissolved and suspended MMs in the snow cover of the western part of Moscow were identified by cluster analysis (Figure 6). Seven MMs associations were distinguished for dissolved forms, i.e., Cl-Na-Sr-Ca (r = 0. 86 [75]. Their consumption for single road treatment is 80-200 g/m 2 [116]. Moscow community services apply liquid DISs at temperatures higher than −16 • C; at lower temperatures, combined ones are applied, which include marble chips (up to 50-60%), and crystals of calcium chloride and formic acid salts. The solubility of marble is low, but it increases with diminishing size of its chips in the presence of dissolved calcium chloride and pavement particles [70]. Only combined DISs are approved for application in the yards, grounds surrounding residential buildings, sidewalks, and pedestrian streets of Moscow. DISs and the construction dust of carbonate composition could also be a source of Sr, since this metal is often contained in Ca and Mg carbonates [117]. Large amounts of MMs accumulate in snow cover as a result of soil and road dust particles transfer. They are resuspended from the road surface during long snowless periods and from the snow-free areas [4], as well as when cars spray particles of contaminated material accumulated on the road surface and consisting of snow, DISs, dirt from the car wheels, and a large mass of soil particles [21]. Input of a large group of MMs as a result of blowing and splashing mud material from the surface of roads is indicated by the formation of associations of suspended Ni-Al-Mg-Ti-Ca-Sr-Mn-Co-W-K-Rb-Ba-Ni-Fe-V and dissolved Ti-Fe-Pb-Al-Sn-Bi-W. Thus, Al, Ti, Fe, Mn, Rb, and K come predominantly with soil particles upon blowing [118][119][120]; Na, Ca, Mg, and Sr-with construction dust and large DISs particles; W, Sn, Bi, Co, Ni, Ba, Pb, and Ti-with various size fractions of road dust [67,95,119,[121][122][123][124][125].
The input of elements into snow cover from roadside areas is difficult to separate from their entry with car emissions, since both road dust and roadside soils are partly polluted with MMs by vehicles emissions. Therefore, wear of brake pads and other metal parts of vehicles leads to the formation of associations of dissolved Cr-Ba-Ni and suspended Cr-Zn, and probably dissolved Mo-Sb-SO 4 2together with suspended Sn-Bi and Mo-Sb-Cd-As in roadside snow. The assumption is supported by the results of studies in which Ba, Zn, Sb, Sn, Mo, Bi, Cr, and Ni were proved to be indicator elements for such effects of motor vehicles [91,93,118,120,[126][127][128][129][130]. Ba and Sb sulphates used as a friction modifier in the production of brake linings [131], as well as antimony sulfide (III)-Sb 2 S 3 , which is a component of brake lubricant [92] could be sources of sulfate ion in snow cover. Vehicle exhausts contribute to the formation of dissolved K-NO3 -association in roadside snow cover. Most commonly, the input of K is attributed to the combustion of organic residues, biomass, or coal [132][133][134]. However, there are no significant sources of biomass combustion within the WAO territory, and power plants burn mainly natural gas in winter, so the input of K and NO3 − from vehicles seems more likely. Moreover, significant correlations of NO3 -with dissolved Cu (r = 0.62) and Rb (r = 0.42), and of dissolved K with dissolved forms of Rb (r = 0.75), Cu (r = 0.64), Sr (r = 0.52), Co (r = 0.52), W (r = 0.47), Cl (r = 0.41), and Na (r = 0.39) are typical of snow cover in WAO. This may indicate additional input of K and NO3 -with DISs (in the form of KCl, or as impurities to the DISs of chloride composition), as well as when blowing and splashing road dust and soil particles, sometimes with admixed potassium and nitrogen fertilizers.
The anthropogenic impact of industrial enterprises in the western part of Moscow is less intense than that of vehicles, but this source could contribute to the formation of dissolved Mo-Sb-SO4 2− Abrasion of tires and the roadway surface causes the formation of the association of dissolved Mn-Cd-Cu-Co-Rb in roadside snow cover of the Moscow WAO. These MMs are often used as indicators of this type of transport impact [89,93,118,126,127]. In addition, Zn, Cr, Mo, and Sb are indicators of tire abrasion [122,127], while Cu, Cd, and Mn indicate brake pads and linings wearing [89,119,121,122,126]. However, the consideration of brake pads abrasion and tire wear as separate factors is rather questionable because they form a wide range of MMs associations. Therefore, the abrasion of brake pads and tires is sometimes classified as a single "vehicle abrasion" factor [118].
Vehicle exhausts contribute to the formation of dissolved K-NO 3 association in roadside snow cover. Most commonly, the input of K is attributed to the combustion of organic residues, biomass, or coal [132][133][134]. However, there are no significant sources of biomass combustion within the WAO territory, and power plants burn mainly natural gas in winter, so the input of K and NO 3 − from vehicles seems more likely. Moreover, significant correlations of NO 3 with dissolved Cu (r = 0. 62) and Rb (r = 0.42), and of dissolved K with dissolved forms of Rb (r = 0.75), Cu (r = 0.64), Sr (r = 0.52), Co (r = 0.52), W (r = 0.47), Cl (r = 0.41), and Na (r = 0.39) are typical of snow cover in WAO. This may indicate additional input of K and NO 3 with DISs (in the form of KCl, or as impurities to the DISs of chloride composition), as well as when blowing and splashing road dust and soil particles, sometimes with admixed potassium and nitrogen fertilizers. The anthropogenic impact of industrial enterprises in the western part of Moscow is less intense than that of vehicles, but this source could contribute to the formation of dissolved Mo-Sb-SO 4 2− association in snow cover. Despite the fact that Moscow thermal power plants burn mainly natural gas during the heating season, fuel oil is also used there during severe and prolonged frosts as an additional fuel. This contributes to higher SO 2 emissions into the atmospheric air [77] and, probably, increases SO 4 2− concentrations in snow cover.
Both the dissolved forms of V and Zn, and suspended forms of Cu and Pb could come in different amounts from all the above-discussed sources. Thus, no close associations with other MMs were found for these elements.

Conclusions
The undertaken studies proved the significant impact of motor transport, industrial facilities, and DISs on urban snow cover pollution. The obtained data made it possible to define in detail the snow cover pollution pattern of snow over in the western part of Moscow, which could be used to predict the after-snowmelt fate of MMs in other urban environments.
In the western part of Moscow, anthropogenic impact caused a significant increase of dust load (2-7 times), concentration of solid particles in snow cover (2-5 times), mineralization of snow meltwater (5-18 times), and the change of its ionic composition from calcium bicarbonate to calcium-sodium chloride (as compared with background snow cover).
Suspended forms of Ca, W, Co, V, Sr, Ti, Mg, Na, Mo, Zn, Fe, Sb, and Cu are primary pollutants in the traffic zone of the western part of Moscow; their concentrations in roadside snow cover are more than 25 times in excess over the background. Na, Sr, Ca, K, Mo, Sb, and W dominate among the dissolved forms, with six and more times excess over the background. The location of the anomalies of dissolved and suspended MMs concentrations matches those of the deposition of mentioned MMs forms in snow cover within the WAO. These anomalies are localized near the MRR and many large and medium roads. Na is the most important pollutant; its contribution to total deposition of pollutants increases with growing amount of DISs application-from 38-45% at the MO MSU and in the yards to 51-68% on the roads.
In WAO, the following anthropogenic sources supply different groups of chemical elements that form specific paragenetic associations of MMs in snow cover: DISs (dissolved Cl-Na-Sr-Ca