# Long-Term Dynamics of Urban Soil Pollution with Heavy Metals in Moscow

Authors: N. E. Kosheleva; E. M. Nikiforova
Journal: Applied and Environmental Soil Science
 (2016)

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## Abstract

Results of 21-year-long (1989–2010) observations of the concentrations and the spatial distribution patterns of nine heavy metals (HMs) in topsoils of the Eastern district of Moscow are presented. The quantitative parameters of soil pollution include the annual increase rates of HM concentrations in several land-use zones. The maps of geochemical anomalies were compiled using the data collected in 1989, 2005, and 2010. The growth of the total volume of industrial and vehicles’ emissions between 1989 and 2005 caused significant deposition of Pb, Zn, Cu, and Cd. The additional input of Cd to the soils is attributed to the application of sewage sludge as fertilizers. The relative increment of concentrations was the highest for Pb, Co, Cu, Ni, and Cr. In 2005–2010, the relative annual increment rate was the highest for Cr, Cd, Co, and Ni, and it increased by an order of magnitude as compared to the previous period. By contrast, Pb and Cu concentrations decreased owing to the soil reclamation, the exclusion of leaded gasoline as a fuel for vehicles and closing some hazardous enterprises. Joint analysis of snow and soil geochemical maps allows identification of the zones of actual, permanent, and relict pollution.


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## Body

## 1. Introduction

Development of industrial cities and rapid growth of urban population aggravates ecological problems caused by air and water contamination and permanent accumulation of pollutants in soils. Heavy metals (HMs) are of special concern since they belong to very hazardous substances. The content and distribution of HMs in Moscow soils have been analyzed by many authors [1–7]. At the same time, such urgent issues of urban ecology as a long-term dynamics of soil contamination with HMs in different land-use zones have not yet been considered. The aim of this research is to study spatial-temporal trends in soil contamination with HMs in one of the most polluted districts of Moscow.The specific purposes of the study are as follows:(i)
to investigate the main features of long-term dynamics of HM content in the soil cover in relation to land-use type and fluctuations in urban activities;
(ii)
to map technogenic geochemical anomalies in urban soils for different time periods;
(iii)
to determine the character and intensity of HM accumulation in urban soils by combined analysis of snow and soil geochemical maps;
(iv)
to evaluate the environmental risk of the contamination on the basis of integral indices.


## 2. Materials and Methods

The Eastern district has been chosen as a study object; it is located on the Meshchera outwash plain. The southern, most polluted, part of the Moscow Eastern district was investigated. This territory belongs to the southern taiga Meshchera landscapes with a temperate continental climate. The snow cover appears in late October–early January and reaches the maximum height in February-March. A flat plain with altitudes of 150–160 m a.s.l. is composed of glaciofluvial sands and loams with low content of HMs [8]. Soil cover has been severely disturbed; natural sod-podzolic, podzolic-bog, and bog soils are preserved only locally in the suburbs and green areas. The major part of the area is occupied by specific urban soils, that is, urbanozems and technozems [9], developed on filled redeposited substrates and the cultivated layer; in some parks and recreation zones, soils develop on the natural parent rocks.The most widespread soils are urbanozems that are deeply transformed anthropogenic soils, the profiles of which change to a depth of more than 50 cm. Their main difference from natural soils is the presence of a diagnostic “urbic” horizon. This surface horizon is a filled mixed layer with an admixture (>5%) of anthropogenic inclusions (construction and industrial waste, domestic garbage); as a rule, it contains organic matter. The physical and chemical properties of this horizon change owing to the input of eolian dust [5].The territory has multispecialized industries, including instruments and equipment producing, chemical and oil-processing factories, heating power stations, incineration plant, and a dense network of roads. Highways are the Moscow Ring Road (MKAD) and Shosse Entuziastov. Motor transport is the main source of pollution in the district [10]. The largest industrial zones are Karacharovo and Sokolinaya Gora in the north-east of the study area; Perovo in the center; Vykhino and Gaivoronovo in the south. Owing to the fall in production and decrease in the volume of wastes and emissions, the input of stationary air pollution sources decreased from 26-27% of the total mass of technogenic load, in the early 1990s to 10% at the end of the decade [11]. Nevertheless Moscow still ranks 10th–13th among Russian cities by the total pollution level from stationary sources; industry remains the most important factor responsible for the contamination of the urban environment with specific emissions.The geochemical studies and soil sampling were performed during the summers of 1989, 2005, and 2010 at the same points (Figure1). Samples were collected at approximately uniform grid with a sampling spacing of 700–900 m. This scheme is widely used in the world for geochemical mapping of cities [13]. Altogether 153 soil mixed samples were taken from the most humus enriched and contaminated upper (0 to 15 cm) horizons of the urban soils. Mixed samples were composed of 4 individual ones. Soddy-podzolic soils of the Meshchera Plain (45–50 km east of the city, where its influence was not displayed) were studied as background analogues. These light-textured soils develop under meadow grass-forb and forest spruce-birch communities. Ten samples were taken from the surface horizons of the reference soils. The bulk content of Zn, Cd, Pb, Cu, Cr, Co, Ni, Mn, and Cs was determined by atomic absorption spectrometry using an Hitachi 180–70 spectrometer. To determine all the elements soil samples were transferred into the state of the solution using the mixture of acids HCl, HClO4, and HNO3, with triple evaporation and complexation of HF with boric acid. The residue was then dissolved in HCl.Figure 1
The map of land-use zones for the territory of the Eastern district of Moscow [12].The type of land use is of primary importance for the formation of technogenic geochemical anomalies; therefore land-use zoning of the territory was performed using satellite high-resolution images [12]. The following areas were specified (Figure 1): highways and industrial zones, medium-rise residential blocks within MKAD, recreation zone (parks, forest parks, and leisure areas), new high-rise buildings (Novokosino, Kozhukhovo), old residential blocks (private low-rise buildings in Novoukhtomskii, Kosino, and Rudnevo settlements), and agricultural area (arable lands of the former Mossovet sovkhoz). The zones differ in duration and intensity of anthropogenic stress. Geochemical maps were compiled using spline interpolation (Geostatistical Analyst, ArcGIS 10).The accumulation or dispersion of dust and HMs in urban soils was evaluated using enrichment or depletion factors estimated via comparison with the data on the HM concentrationsC
f in the reference soddy-podzolic soils: E
F
=
C
/
C
f and D
F
=
C
f
/
C, where C is the element concentration in urban soils. The results are displayed on a special plot namedgeochemical spectrum. The immission of the solid fraction of HMs to soil D equals the dust load P
n in the snow multiplied by HM concentration in it; D
=
P
n
·
C
. Exceedance of HM fallout above background values D
f is characterized by a factor K
d
=
D
/
D
f. Total multielemental pollution of snow and soil cover is defined by integral indices of immission Z
d
=
∑
i
=
1
n
K
d
-
(
n
-
1
) and total pollution Z
c
=
∑
i
=
1
n
E
F
-
(
n
-
1
), respectively, where n is number of elements with K
d or EF > 1. They summarize the excess of the HM contents in urban soils over background levels and thus display the degree of their anthropogenic geochemical transformation [14, 25, 26]. Integral indices have 5 levels which determine the degree of pollution (Table 1). Maps of these parameters reveal spatial patterns of pollution in these depositing media.Table 1
Levels of landscape pollution with HMs and dust [14].
Levels of pollution
Dust depositionP
n, kg/km2 per day
Total indices of
HM immissionZ
d
Snow pollutionZ
c
Soil pollutionZ
c
Low
<200
<1000
<32
<16
Medium
200–300
1000–2000
32–64
16–32
High
300–500
2000–4000
64–128
32–64
Very high
500–800
4000–8000
128–256
64–128
Maximum
>800
>8000
>256
>128


## 3. Results and Discussion

### 3.1. Accumulation of HMs in Urban Soils

The intensity of HM accumulation in the soils of the Eastern district (Figure2) was evaluated in relation to the background soils of Meshchera plain which have trace-level concentrations of all HMs under study, except for Cd and Cs. Low values of metal concentrations in background soils are explained by their contents in parent fluvioglacial sands [8] and the small intensity of fallout from the atmosphere [2, 9].Figure 2
Geochemical spectra of urban soils in the Eastern district of Moscow showing enrichment and depletion factors (EF, DF) of metals in relation to background soils.In 1989 the group of four elements accumulated in urban soils with the following sequence according to their enrichment factors EF (inferior indices): Pb4.4Zn3.7Cu1.7Cd1.4. Other metals dissipated with intensity which was defined by their depletion factors DF (top indices): Cо2.3Mn1.4Cr1.3Cs1.2Ni1.1. The content of HMs in urban soils was very variable; coefficients of variation CV of particular HMs changed from 41 to 89%, reaching 102% for Cd because of differences between the individual land-use zones.In 2005 metals pollutants showed the increasing content while preserving the above sequence: Pb9.9Zn4.9Cu2.6Cd1.8. During 1989–2005 the average concentrations of two main pollutants, Pb and Zn, increased by a factor of 2.2 and 1.3, respectively. The content of Cr, Cs, and Ni came close to their background levels; only Co and Mn had concentrations below the background values (DF 1.6 and 1.2). Soil concentrations of all HMs under study were slightly less variable than in 1989 (CV 32–66% for Co, Ni, Mn, Cs, Zn, Cr, and Cu and 91-92% for Cd and Pb).In 2010, 21 years after the beginning of investigations, further growth of soil pollution with HMs was observed, and the group of metals concentrated in topsoils was expanded up to seven elements. According to EF values, they form the following sequence: Pb6.8Zn5.0Cd4.7Cr3.1Cu2.3Ni2.0 Co1.3. Mn and Cs have the contents below background (DF 1.2 and 2.8, resp.). Since Cs is concentrated in hydroxides of Mn, its removal (washout) from the topsoils is accompanied by a significant decrease in the content of Cs [27]. The concentration of Pb—the main pollutant—decreased by a factor of 1.4 in comparison to 2005 that could be the result of soil reclamation in combination with the exclusion of leaded gasoline as a fuel for vehicles and the closing some hazardous enterprises which produced machines and electronic equipment. The intensive growth of Cd content in urban soils is caused by its presence in the motor vehicle emissions; in agricultural and recreation zone it is related to the application of large amounts of mineral and organic fertilizers and sewage sludge which contain Cd as an admixture. Concentrations of other metals increased slightly or remained at the same level. The contents of Co, Cs, and Pb in soils became less variable, while that of Zn and Cr increased up to 68–70% and of Cd, up to 136%.


### 3.2. HM Content in Soils with Different Type of Land Use

Distinctions in the levels of HM concentration in soils of different land-use zones were revealed through the analysis of values in Table2. Differences in mean HM content were evaluated by t-test. They were significant at P 90–95% for the majority of the elements and land-use zones since mixed samples which were composed of 4 individual ones were used. In 1989 Pb and Zn were accumulated in soils of all land-use zones, particularly within old low-rise residential areas (EF 8.0 and 3.7, resp.), near highways (6.7 and 6.0), and agricultural areas (5.0 and 2.6). The third priority pollutant—Cu—was mostly accumulated in the industrial and transport zones (2.9). Soils of the recreational zone and new high-rise residential areas showed low contents of HMs. Among them the greatest dispersion of Cr (DF 3.5 and 2.0) and Co (2.7 and 4.1, resp.) in comparison with background soils was observed.Table 2
Mean content of HMs (mg/kg) in topsoils of natural background and various land-use zones in the Eastern district of Moscow in 1989, 2005, and 2010.
Year (number of samples)
Pb
Zn
Cu
Cd
Co
Cr
Ni
Mn
Cs
Natural background of the Meshchera lowland
1989 (10)
9.04
37.5
27.9
0.34
6.60
32.0
15.2
585
5.40
Highways (А) and industrial zones (P)
1989 (12)
60.5
224
80.7
0.65
3.85
34.0
17.6
442
5.58
2005 (14)
174
305
130
0.81
5.82
51.7
26.9
518
8.08
2010 (13), А
59.5
183
67.5
1.23
8.48
89.9
32.2
412
1.90
2010 (5), Р
114
286
88.0
1.37
9.3
92.2
35.4
513
1.88
Residential zone with low-rise buildings (L)
1989 (5)
72.4
138
39.4
0.64
2.67
32.1
16.2
463
4.53
2005 (5)
159
180
65.7
0.81
3.84
47.9
22.6
549
6.34
2010 (5)
68.8
163
60.6
1.33
8.12
95.6
33.6
544
1.64
Residential zone with medium-rise buildings (M)
1989 (16)
23.4
130
40.1
0.35
2.48
20.5
12.1
340
4.65
2005 (17)
39.9
165
58.8
0.48
3.76
29.2
17.8
414
6.47
2010 (10)
66.7
223
62.3
1.43
8.6
106
30.0
493
2.09
Residential zone with high-rise buildings (H)
1989 (5)
16.4
76.5
24.6
0.14
1.61
16.3
9.14
260
2.43
2005 (5)
20.2
88.3
28.1
0.15
1.82
18.2
10.6
309
2.91
2010 (7)
44.1
162
54.0
1.45
8.57
104
26.1
389
1.99
Recreational zone (R)
1989 (6)
21.1
76.7
24.3
0.17
2.44
9.24
7.58
512
4.04
2005 (6)
32.9
82.7
28.9
0.20
2.87
11.6
9.20
538
4.44
2010 (9)
49.4
147
50.4
2.05
8.8
101
29.0
482
1.87
Agricultural landscapes (AG)
1989 (5)
45.6
96.3
57.7
1.07
3.20
34.0
18.0
535
3.74
2005 (5)
84.7
122
71.2
1.44
4.09
37.9
21.5
640
5.19
2010 (3)
34.0
173
67.0
3.70
7.7
137
27.3
492
1.47In 2005 the overall picture of HMs distribution in the soils of individual zones was the same, but the concentrations of main pollutants—Pb and Zn—significantly increased (Table2). The highest concentrations were found in the soils of highways and industrial zone (EF 19.2 and 8.1, resp.), old residential blocks (17.6 and 4.8), and agricultural areas (9.4 and 3.3). Low concentrations of the majority of HMs (Co, Cr, Cd, Ni, Mn, and Cs) in comparison with background values were observed in the soils of recreational zone and new high-rise residential quarters (DF 3.6–1.1).In 2010 geochemical contrasts in the soils of individual land-use zones became less pronounced. The concentrations of Cr, Co, and Mn increased in comparison with 2005 practically in all land-use zones, and those of Pb, Cu, Zn decreased in transport and industrial zones, old residential and agricultural areas (except for Zn). The content of Pb in these zones decreased by a factor of 2.3–2.5 that is apparently related to the soil reclamation, as well as to improvement of fuel and changes of vehicle structure. The content of Cd sharply increased, especially in the soils of recreational and agricultural zones. This could be explained by the application of high doses of sewage sludge and phosphoric fertilizers.


### 3.3. Long-Term Dynamics of HM Anomalies in Urban Soils

The time-spatial patterns of HMs distribution in soils are presented on the maps ofZ
c index compiled for several years of the 21-year-long period of observations (Figure 3). In 1989 the territory was characterized by low level of total pollution (Z
c < 16) as a result of rather weak industrial and transport influence on urban soils. On this background there were several small spots of low-contrast technogenic anomalies of HMs with medium level of pollution located in northwest, southeast, and central parts of the district. In the centers of these anomalies the values of Z
c indicator did not exceed 32–35.Figure 3
Total technogenic anomalies of HMs (according toZ
c index) in topsoils of the Eastern district of Moscow in 1989, 2005, and 2010.
(a)
(b)
(c)In 2005 the existing anomalies of HMs in soil cover of the district considerably increased their size and contrast; the total pollution of soils increased by a factor of 1.7 for the 16-year period. The most contrast technogenic anomaly of HMs withZ
c about 48 in its center was formed in the northwest under the influence of emissions from the large industrial zone “Sokolinaya Gora” and Shosse Entuziastov Highway. Several anomalies along the Moscow Ring Road (MKAD at Figure 1) which were poorly expressed in 1989 became larger with maximum Z
c 32–40. Southeast anomaly of HMs in soils also became more pronounced, up to Z
c 48. Thus, the pollution level in anomalies has changed from the medium to high.In 2010 a further increase in the areas and intensity of HM anomalies was observed. The northwest anomaly with the total index of soil pollutionZ
c 48–80 expanded beyond the industrial zone “Sokolinaya Gora” and partly covered residential areas to the south of Shosse Entuziastov Highway. In the center of the district large anomaly with Z
c > 100 was formed under the influence of the industrial zone “Perovo” and district heating station (DHS) “Perovskaya.” In the southeast part of the district technogenic anomaly of HMs was extended to the east while the Z
c indicator increased up to 50–70. It is the result of emissions of recently constructed incineration plant near the settlement of Rudnevo.Growing contamination of urban soils with HMs is caused not only by an increase in emissions from industry and transport in particular, but also by a change in absorption capacity of the soils. Anthropogenic transformation of the physical and chemical properties of the soils leads to the formation of complex physical and chemical barriers. They arise as a result of precipitation of carbonate construction dust enriched by fine particles, application of soil peat compost mixtures with a high content of humic substances for planting of greenery as well as flooding and soil sealing which alters its gas and redox regimes. The HM accumulation on these man-made barriers is not necessarily accompanied by a reduction in their mobility; analysis of mobile forms of HMs showed that their precipitation from the atmosphere exceeds the speed of their washout from topsoils [28].


### 3.4. Trends of HM Accumulation in Topsoils and Snow Cover

Tendencies of HM accumulation in the urban soils were evaluated for two periods: 1989–2005 and 2005–2010 by calculation of average annual growth of HM content in the topsoils (Table3) which differ considerably depending on the type of land use (Figure 4).Table 3
Mean surplus/decrease rate of HM contents in topsoils of the Eastern district of Moscow.
Period
Increment rate
Pb
Zn
Cu
Cd
Co
Cr
Ni
Mn
Cs
1989–2005
mg/kg per year
3.1
2.8
1.6
0.01
0.08
0.64
0.36
4.40
0.11
%
0.08
0.03
0.04
0.03
0.04
0.03
0.03
0.02
0.03
1989–2005
mg/kg per year
−5.4
1.2
−2.1
0.20
0.90
13.0
2.2
3.8
−0.86
%
−0.36
0.03
−0.15
0.89
0.71
0.97
0.45
0.04
−1.1Figure 4
Average increase or reduction of the content of Pb, Cd, Zn, and Cr in the topsoils of different land-use zones in the Eastern district of Moscow for two periods of observations (1989–2005 and 2005–2010). Symbols of land-use zones are given in Table2.From 1989 to 2005 the growth of HM content in soils of the Eastern district was relatively small. The maximum absolute increase was inherent of Mn (4.4 mg/kg per year) > Pb (3.1) > Zn (2.8) > Cu (1.6) > Cr (0.64). Thus, the relative rate was the greatest for Pb, Co, Cu, Ni, and Cr (0.07–0.03% per year) in the soils of industrial zones and near highways, old low-rise residential quarters, and agricultural areas (Figure4).In 2005–2010, the rates of HM accumulation in the soils increased and became more differentiated among the land-use zones (Figure4). Depending on the average annual values HMs form the following sequence: Cr (13.1 mg/kg per year) > Mn (3.8) > Ni (2.2) > Zn (1.2) > Co (0.9). Cr, Cd, Co, and Ni had the maximum relative rate of growth (up to 0.5–1.0%), in comparison with the previous period it increased by tens times (Table 2). The content of Pb, Cs, and Cu significantly decreased showing negative values of the annual rate mainly owing to soil reclamation.Uneven distribution of HM accumulation rates within the territory of the district is well seen on Figure4. Cr and Cd show the overall growth, especially in less polluted zones (recreational, agricultural, and new residential areas), while Pb and Zn dissipate in the soils of industrial zones and highways, old low-rise residential and agricultural areas.The dynamics of soil pollution was compared with the distribution of HMs in the snow. The snow cover reflects actual state of the environment while the soil represents more stable long-term pollution. Joint analysis of snow and soil geochemical maps allows identification of the areas of actual, permanent, and relict pollution. The relict technogenic anomalies occur only in soil cover, modern ones, only in snow, and permanent ones in snow and soils simultaneously [25]. The snow pollution with HMs in the Eastern district of Moscow was defined using the integral index of immission Z
d [29]. It characterizes both the composition and amount of dust which accumulates in snow. Overlay of the maps of Z
c and Z
d integral indices resulted in the identification of permanent anomalies within the major part of the district (Figure 5). In the center of the area a relict anomaly was formed as a result of elimination and reprofiling of the stationary sources of emissions. On the north, along the Shosse Entuziastov Highway a modern anomaly of HMs was discovered in the vicinity of Terletskiy park.Figure 5
Location of areas of actual, permanent, and relict pollution in the Eastern district of Moscow according to anomalies in soils and snow cover.


### 3.5. Assessment of Environmental State of Urban Soils

The analysis of average zonal values of the total indicator of pollutionZ
c (Table 4) showed that in 1989 the most part of the territory under study was characterized by a low level of HM pollution. The average value of Z
c was only 9.0 that indicates harmless ecological condition of soils. Z
c values exceeded this level only in 10 of 49 sampling sites (i.e., 20.4%), mainly in the industrial zones and near highways.Table 4
Long-term dynamics of total HM pollution of soils in the Eastern district of Moscow depending on the type of their use.
Observation year
Average values of total index of pollutionZ
c in soils of the land-use zones
Highways
Industrial
Medium-rise residential
High-rise residential
Recreational
Low-rise residential
Agricultural
Total for the district
1989
15.6
6.3
2.9
3.5
13.2
10.4
9.02
2005
33.4
10.3
3.7
5.0
25.5
17.2
17.3
2010
17.9
28.3
20.4
15.4
17.9
18.6
22.9
19.4In 2005 much less sampling points showedZ
c values < 16 (31 of 52, i.e., 59.6%). Moreover, 14 points (26.9%) shifted to medium and 7 points (13.5%) to high level of pollution. Average Z
c value for the district was 17.3 that corresponds to medium level of HM pollution of soils. There were only three land-use zones with low level of soil contamination, residential zones with medium- and high-rise buildings, and recreational zone (Table 4). In 2005 soils of the residential low-rise zone and agricultural landscapes had medium level of HM pollution, and those of highways and industrial zones had high one.In 2010 the averageZ
c value for the district increased up to 19.4. In contrast to the decrease of soil pollution level for highways, industrial and residential zones with low-rise buildings, a significant increase of HM pollution occurred in recreational, agricultural, and residential high-rise zones. Thus it is only in the latter zone where the level of soil contamination corresponds to harmless category; other zones are moderately polluted (Z
c 17.9–28.3).To assess the ecological rank of Moscow in terms of the level of HM accumulation in soils among the cities of the world, we compared the average contents of four most common HMs (Pb Zn, Cr, and Ni) in the soils of large and capital cities of several countries with their values in the soils of the Eastern district of Moscow. Soils of the large cities of the world have rather high average HM concentrations (Table5) comparable to Moscow quantities, especially Pb and Zn. Most intensive accumulation of Pb is typical for the soils of London, Naples, Palermo, and Hamburg, while that of Zn is typical for the soils of Hamburg, Naples, Berlin, and Madrid. The contents of Cr and Ni are below their clarks in the lithosphere; the minimum values are observed in the soils of Madrid, Berlin, Palermo, and Stockholm. So, according to 2010 data, soils of the Eastern district of Moscow do not show particularly high levels of HM accumulation. The average content of Pb in the topsoils of the district is close to its values in the soils of Belgrade and that of Zn is close to its values in the soils of Stockholm and London. The same levels of the content of Cr, as in soils of the Eastern district, are recorded in Palermo and Hamburg, and that of Ni is recorded in Seville and Palermo.Table 5
Clarks in the lithosphere [15] and the average contents of Pb, Zn, Cr, and Ni in soils (mg/kg) of the various cities of the world (compiled by the authors according to [16–24] and to own data for the Eastern district of Moscow, 2010).
HM
Lithosphere clark
Stockholm
Madrid
Seville
Berlin
Hamburg
London
Hong Kong
Palermo
Naples
Belgrade
Da Nang
Moscow, Eastern district
Pb
16
101
161
161
119
218
294
93.4
253
262
55.5
20.0
61.8
Zn
83
171
210
107
243
516
183
168
151
251
118
142
189
Cr
83
34.0
74.7
42.8
35.0
95.4
—
<40.0
39.0
74.0
32.1
92.2
100
Ni
58
12.8
14.1
23.5
10.7
62.5
—
<20.0
19.1
—
68.0
22.6
30.6


## 3.1. Accumulation of HMs in Urban Soils

The intensity of HM accumulation in the soils of the Eastern district (Figure2) was evaluated in relation to the background soils of Meshchera plain which have trace-level concentrations of all HMs under study, except for Cd and Cs. Low values of metal concentrations in background soils are explained by their contents in parent fluvioglacial sands [8] and the small intensity of fallout from the atmosphere [2, 9].Figure 2
Geochemical spectra of urban soils in the Eastern district of Moscow showing enrichment and depletion factors (EF, DF) of metals in relation to background soils.In 1989 the group of four elements accumulated in urban soils with the following sequence according to their enrichment factors EF (inferior indices): Pb4.4Zn3.7Cu1.7Cd1.4. Other metals dissipated with intensity which was defined by their depletion factors DF (top indices): Cо2.3Mn1.4Cr1.3Cs1.2Ni1.1. The content of HMs in urban soils was very variable; coefficients of variation CV of particular HMs changed from 41 to 89%, reaching 102% for Cd because of differences between the individual land-use zones.In 2005 metals pollutants showed the increasing content while preserving the above sequence: Pb9.9Zn4.9Cu2.6Cd1.8. During 1989–2005 the average concentrations of two main pollutants, Pb and Zn, increased by a factor of 2.2 and 1.3, respectively. The content of Cr, Cs, and Ni came close to their background levels; only Co and Mn had concentrations below the background values (DF 1.6 and 1.2). Soil concentrations of all HMs under study were slightly less variable than in 1989 (CV 32–66% for Co, Ni, Mn, Cs, Zn, Cr, and Cu and 91-92% for Cd and Pb).In 2010, 21 years after the beginning of investigations, further growth of soil pollution with HMs was observed, and the group of metals concentrated in topsoils was expanded up to seven elements. According to EF values, they form the following sequence: Pb6.8Zn5.0Cd4.7Cr3.1Cu2.3Ni2.0 Co1.3. Mn and Cs have the contents below background (DF 1.2 and 2.8, resp.). Since Cs is concentrated in hydroxides of Mn, its removal (washout) from the topsoils is accompanied by a significant decrease in the content of Cs [27]. The concentration of Pb—the main pollutant—decreased by a factor of 1.4 in comparison to 2005 that could be the result of soil reclamation in combination with the exclusion of leaded gasoline as a fuel for vehicles and the closing some hazardous enterprises which produced machines and electronic equipment. The intensive growth of Cd content in urban soils is caused by its presence in the motor vehicle emissions; in agricultural and recreation zone it is related to the application of large amounts of mineral and organic fertilizers and sewage sludge which contain Cd as an admixture. Concentrations of other metals increased slightly or remained at the same level. The contents of Co, Cs, and Pb in soils became less variable, while that of Zn and Cr increased up to 68–70% and of Cd, up to 136%.


## 3.2. HM Content in Soils with Different Type of Land Use

Distinctions in the levels of HM concentration in soils of different land-use zones were revealed through the analysis of values in Table2. Differences in mean HM content were evaluated by t-test. They were significant at P 90–95% for the majority of the elements and land-use zones since mixed samples which were composed of 4 individual ones were used. In 1989 Pb and Zn were accumulated in soils of all land-use zones, particularly within old low-rise residential areas (EF 8.0 and 3.7, resp.), near highways (6.7 and 6.0), and agricultural areas (5.0 and 2.6). The third priority pollutant—Cu—was mostly accumulated in the industrial and transport zones (2.9). Soils of the recreational zone and new high-rise residential areas showed low contents of HMs. Among them the greatest dispersion of Cr (DF 3.5 and 2.0) and Co (2.7 and 4.1, resp.) in comparison with background soils was observed.Table 2
Mean content of HMs (mg/kg) in topsoils of natural background and various land-use zones in the Eastern district of Moscow in 1989, 2005, and 2010.
Year (number of samples)
Pb
Zn
Cu
Cd
Co
Cr
Ni
Mn
Cs
Natural background of the Meshchera lowland
1989 (10)
9.04
37.5
27.9
0.34
6.60
32.0
15.2
585
5.40
Highways (А) and industrial zones (P)
1989 (12)
60.5
224
80.7
0.65
3.85
34.0
17.6
442
5.58
2005 (14)
174
305
130
0.81
5.82
51.7
26.9
518
8.08
2010 (13), А
59.5
183
67.5
1.23
8.48
89.9
32.2
412
1.90
2010 (5), Р
114
286
88.0
1.37
9.3
92.2
35.4
513
1.88
Residential zone with low-rise buildings (L)
1989 (5)
72.4
138
39.4
0.64
2.67
32.1
16.2
463
4.53
2005 (5)
159
180
65.7
0.81
3.84
47.9
22.6
549
6.34
2010 (5)
68.8
163
60.6
1.33
8.12
95.6
33.6
544
1.64
Residential zone with medium-rise buildings (M)
1989 (16)
23.4
130
40.1
0.35
2.48
20.5
12.1
340
4.65
2005 (17)
39.9
165
58.8
0.48
3.76
29.2
17.8
414
6.47
2010 (10)
66.7
223
62.3
1.43
8.6
106
30.0
493
2.09
Residential zone with high-rise buildings (H)
1989 (5)
16.4
76.5
24.6
0.14
1.61
16.3
9.14
260
2.43
2005 (5)
20.2
88.3
28.1
0.15
1.82
18.2
10.6
309
2.91
2010 (7)
44.1
162
54.0
1.45
8.57
104
26.1
389
1.99
Recreational zone (R)
1989 (6)
21.1
76.7
24.3
0.17
2.44
9.24
7.58
512
4.04
2005 (6)
32.9
82.7
28.9
0.20
2.87
11.6
9.20
538
4.44
2010 (9)
49.4
147
50.4
2.05
8.8
101
29.0
482
1.87
Agricultural landscapes (AG)
1989 (5)
45.6
96.3
57.7
1.07
3.20
34.0
18.0
535
3.74
2005 (5)
84.7
122
71.2
1.44
4.09
37.9
21.5
640
5.19
2010 (3)
34.0
173
67.0
3.70
7.7
137
27.3
492
1.47In 2005 the overall picture of HMs distribution in the soils of individual zones was the same, but the concentrations of main pollutants—Pb and Zn—significantly increased (Table2). The highest concentrations were found in the soils of highways and industrial zone (EF 19.2 and 8.1, resp.), old residential blocks (17.6 and 4.8), and agricultural areas (9.4 and 3.3). Low concentrations of the majority of HMs (Co, Cr, Cd, Ni, Mn, and Cs) in comparison with background values were observed in the soils of recreational zone and new high-rise residential quarters (DF 3.6–1.1).In 2010 geochemical contrasts in the soils of individual land-use zones became less pronounced. The concentrations of Cr, Co, and Mn increased in comparison with 2005 practically in all land-use zones, and those of Pb, Cu, Zn decreased in transport and industrial zones, old residential and agricultural areas (except for Zn). The content of Pb in these zones decreased by a factor of 2.3–2.5 that is apparently related to the soil reclamation, as well as to improvement of fuel and changes of vehicle structure. The content of Cd sharply increased, especially in the soils of recreational and agricultural zones. This could be explained by the application of high doses of sewage sludge and phosphoric fertilizers.


## 3.3. Long-Term Dynamics of HM Anomalies in Urban Soils

The time-spatial patterns of HMs distribution in soils are presented on the maps ofZ
c index compiled for several years of the 21-year-long period of observations (Figure 3). In 1989 the territory was characterized by low level of total pollution (Z
c < 16) as a result of rather weak industrial and transport influence on urban soils. On this background there were several small spots of low-contrast technogenic anomalies of HMs with medium level of pollution located in northwest, southeast, and central parts of the district. In the centers of these anomalies the values of Z
c indicator did not exceed 32–35.Figure 3
Total technogenic anomalies of HMs (according toZ
c index) in topsoils of the Eastern district of Moscow in 1989, 2005, and 2010.
(a)
(b)
(c)In 2005 the existing anomalies of HMs in soil cover of the district considerably increased their size and contrast; the total pollution of soils increased by a factor of 1.7 for the 16-year period. The most contrast technogenic anomaly of HMs withZ
c about 48 in its center was formed in the northwest under the influence of emissions from the large industrial zone “Sokolinaya Gora” and Shosse Entuziastov Highway. Several anomalies along the Moscow Ring Road (MKAD at Figure 1) which were poorly expressed in 1989 became larger with maximum Z
c 32–40. Southeast anomaly of HMs in soils also became more pronounced, up to Z
c 48. Thus, the pollution level in anomalies has changed from the medium to high.In 2010 a further increase in the areas and intensity of HM anomalies was observed. The northwest anomaly with the total index of soil pollutionZ
c 48–80 expanded beyond the industrial zone “Sokolinaya Gora” and partly covered residential areas to the south of Shosse Entuziastov Highway. In the center of the district large anomaly with Z
c > 100 was formed under the influence of the industrial zone “Perovo” and district heating station (DHS) “Perovskaya.” In the southeast part of the district technogenic anomaly of HMs was extended to the east while the Z
c indicator increased up to 50–70. It is the result of emissions of recently constructed incineration plant near the settlement of Rudnevo.Growing contamination of urban soils with HMs is caused not only by an increase in emissions from industry and transport in particular, but also by a change in absorption capacity of the soils. Anthropogenic transformation of the physical and chemical properties of the soils leads to the formation of complex physical and chemical barriers. They arise as a result of precipitation of carbonate construction dust enriched by fine particles, application of soil peat compost mixtures with a high content of humic substances for planting of greenery as well as flooding and soil sealing which alters its gas and redox regimes. The HM accumulation on these man-made barriers is not necessarily accompanied by a reduction in their mobility; analysis of mobile forms of HMs showed that their precipitation from the atmosphere exceeds the speed of their washout from topsoils [28].


## 3.4. Trends of HM Accumulation in Topsoils and Snow Cover

Tendencies of HM accumulation in the urban soils were evaluated for two periods: 1989–2005 and 2005–2010 by calculation of average annual growth of HM content in the topsoils (Table3) which differ considerably depending on the type of land use (Figure 4).Table 3
Mean surplus/decrease rate of HM contents in topsoils of the Eastern district of Moscow.
Period
Increment rate
Pb
Zn
Cu
Cd
Co
Cr
Ni
Mn
Cs
1989–2005
mg/kg per year
3.1
2.8
1.6
0.01
0.08
0.64
0.36
4.40
0.11
%
0.08
0.03
0.04
0.03
0.04
0.03
0.03
0.02
0.03
1989–2005
mg/kg per year
−5.4
1.2
−2.1
0.20
0.90
13.0
2.2
3.8
−0.86
%
−0.36
0.03
−0.15
0.89
0.71
0.97
0.45
0.04
−1.1Figure 4
Average increase or reduction of the content of Pb, Cd, Zn, and Cr in the topsoils of different land-use zones in the Eastern district of Moscow for two periods of observations (1989–2005 and 2005–2010). Symbols of land-use zones are given in Table2.From 1989 to 2005 the growth of HM content in soils of the Eastern district was relatively small. The maximum absolute increase was inherent of Mn (4.4 mg/kg per year) > Pb (3.1) > Zn (2.8) > Cu (1.6) > Cr (0.64). Thus, the relative rate was the greatest for Pb, Co, Cu, Ni, and Cr (0.07–0.03% per year) in the soils of industrial zones and near highways, old low-rise residential quarters, and agricultural areas (Figure4).In 2005–2010, the rates of HM accumulation in the soils increased and became more differentiated among the land-use zones (Figure4). Depending on the average annual values HMs form the following sequence: Cr (13.1 mg/kg per year) > Mn (3.8) > Ni (2.2) > Zn (1.2) > Co (0.9). Cr, Cd, Co, and Ni had the maximum relative rate of growth (up to 0.5–1.0%), in comparison with the previous period it increased by tens times (Table 2). The content of Pb, Cs, and Cu significantly decreased showing negative values of the annual rate mainly owing to soil reclamation.Uneven distribution of HM accumulation rates within the territory of the district is well seen on Figure4. Cr and Cd show the overall growth, especially in less polluted zones (recreational, agricultural, and new residential areas), while Pb and Zn dissipate in the soils of industrial zones and highways, old low-rise residential and agricultural areas.The dynamics of soil pollution was compared with the distribution of HMs in the snow. The snow cover reflects actual state of the environment while the soil represents more stable long-term pollution. Joint analysis of snow and soil geochemical maps allows identification of the areas of actual, permanent, and relict pollution. The relict technogenic anomalies occur only in soil cover, modern ones, only in snow, and permanent ones in snow and soils simultaneously [25]. The snow pollution with HMs in the Eastern district of Moscow was defined using the integral index of immission Z
d [29]. It characterizes both the composition and amount of dust which accumulates in snow. Overlay of the maps of Z
c and Z
d integral indices resulted in the identification of permanent anomalies within the major part of the district (Figure 5). In the center of the area a relict anomaly was formed as a result of elimination and reprofiling of the stationary sources of emissions. On the north, along the Shosse Entuziastov Highway a modern anomaly of HMs was discovered in the vicinity of Terletskiy park.Figure 5
Location of areas of actual, permanent, and relict pollution in the Eastern district of Moscow according to anomalies in soils and snow cover.


## 3.5. Assessment of Environmental State of Urban Soils

The analysis of average zonal values of the total indicator of pollutionZ
c (Table 4) showed that in 1989 the most part of the territory under study was characterized by a low level of HM pollution. The average value of Z
c was only 9.0 that indicates harmless ecological condition of soils. Z
c values exceeded this level only in 10 of 49 sampling sites (i.e., 20.4%), mainly in the industrial zones and near highways.Table 4
Long-term dynamics of total HM pollution of soils in the Eastern district of Moscow depending on the type of their use.
Observation year
Average values of total index of pollutionZ
c in soils of the land-use zones
Highways
Industrial
Medium-rise residential
High-rise residential
Recreational
Low-rise residential
Agricultural
Total for the district
1989
15.6
6.3
2.9
3.5
13.2
10.4
9.02
2005
33.4
10.3
3.7
5.0
25.5
17.2
17.3
2010
17.9
28.3
20.4
15.4
17.9
18.6
22.9
19.4In 2005 much less sampling points showedZ
c values < 16 (31 of 52, i.e., 59.6%). Moreover, 14 points (26.9%) shifted to medium and 7 points (13.5%) to high level of pollution. Average Z
c value for the district was 17.3 that corresponds to medium level of HM pollution of soils. There were only three land-use zones with low level of soil contamination, residential zones with medium- and high-rise buildings, and recreational zone (Table 4). In 2005 soils of the residential low-rise zone and agricultural landscapes had medium level of HM pollution, and those of highways and industrial zones had high one.In 2010 the averageZ
c value for the district increased up to 19.4. In contrast to the decrease of soil pollution level for highways, industrial and residential zones with low-rise buildings, a significant increase of HM pollution occurred in recreational, agricultural, and residential high-rise zones. Thus it is only in the latter zone where the level of soil contamination corresponds to harmless category; other zones are moderately polluted (Z
c 17.9–28.3).To assess the ecological rank of Moscow in terms of the level of HM accumulation in soils among the cities of the world, we compared the average contents of four most common HMs (Pb Zn, Cr, and Ni) in the soils of large and capital cities of several countries with their values in the soils of the Eastern district of Moscow. Soils of the large cities of the world have rather high average HM concentrations (Table5) comparable to Moscow quantities, especially Pb and Zn. Most intensive accumulation of Pb is typical for the soils of London, Naples, Palermo, and Hamburg, while that of Zn is typical for the soils of Hamburg, Naples, Berlin, and Madrid. The contents of Cr and Ni are below their clarks in the lithosphere; the minimum values are observed in the soils of Madrid, Berlin, Palermo, and Stockholm. So, according to 2010 data, soils of the Eastern district of Moscow do not show particularly high levels of HM accumulation. The average content of Pb in the topsoils of the district is close to its values in the soils of Belgrade and that of Zn is close to its values in the soils of Stockholm and London. The same levels of the content of Cr, as in soils of the Eastern district, are recorded in Palermo and Hamburg, and that of Ni is recorded in Seville and Palermo.Table 5
Clarks in the lithosphere [15] and the average contents of Pb, Zn, Cr, and Ni in soils (mg/kg) of the various cities of the world (compiled by the authors according to [16–24] and to own data for the Eastern district of Moscow, 2010).
HM
Lithosphere clark
Stockholm
Madrid
Seville
Berlin
Hamburg
London
Hong Kong
Palermo
Naples
Belgrade
Da Nang
Moscow, Eastern district
Pb
16
101
161
161
119
218
294
93.4
253
262
55.5
20.0
61.8
Zn
83
171
210
107
243
516
183
168
151
251
118
142
189
Cr
83
34.0
74.7
42.8
35.0
95.4
—
<40.0
39.0
74.0
32.1
92.2
100
Ni
58
12.8
14.1
23.5
10.7
62.5
—
<20.0
19.1
—
68.0
22.6
30.6


## 4. Conclusions

Soils of the Eastern district of Moscow show the gradual increase of HM pollution levels. Among them Pb and Zn are the leaders with enrichment factors EF 3.7–9.9. In 2010 Cd joined them (EF 4.7); the intensive growth of its content is caused by its presence in the motor vehicle emissions as well as by application of mineral and organic fertilizers and sewage sludge containing Cd as an admixture. Over the last 5 years the contents of Pb and Cu in soils of the district decreased owing to the soil reclamation and adding uncontaminated material, the exclusion of leaded gasoline as a fuel for vehicles, and also conversion and closing a number of hazardous industrial enterprises which emit these metals.In 1989–2005 the annual increase of HM concentrations in soils of the Eastern district was rather low. Pb and Cu demonstrated the maximum rates of increase (0.08 and 0.04% per year, resp.). In 2005–2010 rates of the annual increase of HM concentrations in soils were higher, with more pronounced differentiation in particular land-use zones. Cr, Cd, Co, and Ni had the maximum rates of increase (1.0–0.45% per year). The contents of Pb and Cu in the soils of industrial zones and highways, agricultural, and old residential areas went down. Nevertheless, these zones still have the highest contents and the widest range of elements pollutants.At present, a medium total pollution level is common for the soils of the Eastern district, with theZ
c index reaching 28.3 in the industrial zone. The priority contaminants are Pb, Zn, and Cd. The maximum level of Pb and Zn concentrations (114 and 286 mg/kg, resp.) in topsoils has been revealed in the industrial zone, while that of Cd (3.7 mg/kg) has been revealed in the recreational zone.To represent the stages of development of the technogenic multielemental anomalies in urban soils maps of a total index of pollutionZ
c were compiled for particular years of the 21-year period of observations. Their analysis revealed a significant increase of the contrast and the area of HM anomalies in recent years, which could be attributed to the growth of the total amount of industrial and motor transport emissions and change in absorption capacity of the urban soils.



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*Source: 5602795-2016-03-06.xml*