3.1 Heavy metals concentration
The results of the heavy metals accumulation level in the topsoil and sub soil are presented in Table 1. It was observed that the Cd concentration in the topsoil ranged from 0.144 mg/kg to 0.199 mg/kg with mean of 0.172 mg/kg; while in the subsoil the Cd level ranges from 0.102 mg/kg to 0.163 mg/kg (mean ~ 0.139 mg/kg). The topsoil Cr content varied from 0.224 mg/kg to 0.558 mg/kg, and average value of 0.36 mg/kg; while in the subsoil, the Cr concentration varied from 0.123 mg/kg to 0.462 mg/kg (mean ~ 0.274 mg/kg). Also, the Cu content in the topsoil varied from 0.445 mg/kg to 0.832 mg/kg (mean ~ 0.64 mg/kg); while the Cu level in the subsoil lies between 0.315 mg/kg and 0.595 mg/kg (mean ~ 0.462 mg/kg). The topsoil Fe concentration varied between 121.60 mg/kg and 343.50 mg/kg (average ~ 159.40); while the Fe level in the subsoil ranged from 114.80 mg/kg − 253.10 mg/kg (average ~ 138.90 mg/kg). Additionally, the Pb content of the topsoil lies between 0.316 mg/kg and 0.591 mg/kg (mean 0.415 mg/kg); and the subsoil Pb concentration varied from 0.258 mg/kg − 0.522 mg/kg (mean ~ 0.349 mg/kg). It was detected that the topsoil Mn content ranged between 1.004 mg/kg and 1.994 mg/kg (mean ~ 1.378 mg/kg); and the subsoil Mn concentration varied from 0.885 mg/kg − 1.518 mg/kg (average ~ 1.144 mg/kg). Furthermore, the results shows that the Ni content of the topsoil varied from 0.445 mg/kg − 1.121 mg/kg (mean ~ 0.745 mg/kg), and in the subsoil the Ni level lies between 0.395 mg/kg and 1.005 mg/kg (mean ~ 0.586 mg/kg). Then as for Zn, its concentration in the topsoil ranged from 1.877 mg/kg − 2.553 mg/kg (average ~ 2.184 mg/kg); and its content in the subsoil varied between 1.158 mg/kg and 2.112 mg/kg (mean ~ 1.793 mg/kg). These results are in conformity with Onianwa and Fakayoda (2000) reports which stated that automobile activities caused substantial increment in Zn, Cd, Pb and Ni concentration in the soil
The results further depicted that the concentration level of the metals at the topsoil was higher than the metals accumulation level recorded at the subsoil. This situation could be possibly caused by the higher concentration and amount of leachates the topsoil received, when compared to the subsoil. Mohammed and Abdu (2014) and Darma et al. (2022) reported similar situation of vertical variation of heavy metals concentration in soil samples collected from gold mines areas. Likewise, Ipeaiyeda and Dawodu (2008) stated that concentration of Zn, Cr and Ni declined unevenly as the soil depth increased from 0 m to 0.5 m. According to Adewumi (2020), the lower heavy metals concentration usually obtained at greater soil depth could be attributed to excessive leaching of these elements from this soil stratum.
Generally, Fe had the maximum concentration among all the heavy metals investigated, in the topsoil (159.40 mg/kg) and subsoil (138.90 mg/kg) respectively; while Cd had the minimum concentration among all the heavy metals investigated, in the topsoil (0.172 mg/kg) and subsoil (0.139 mg/kg) respectively. Interestingly, the concentration of the eight (8) heavy metals evaluated at the mechanic workshop’s topsoil and subsoil, were higher when compared to the values obtained at the reference point. This signifies that the effluent discharge from the waste generated by the artisans have significant effect on the soil’s heavy metals concentration. Similar results were obtained by Adelekan and Abegunde (2011), where the Cd, Cu, Pb, Cr and Ni concentration levels in soil samples collected from the vicinity of vehicle maintenance workshops, were considerably higher than the results corded at the reference site.
Table 1
Heavy metal accumulation level in the soil
Soil sample | | Cd | Cr | Cu | Fe | Pb | Mn | Ni | Zn |
Top soil | Minimum | 0.144 | 0.224 | 0.445 | 121.60 | 0.316 | 1.004 | 0.445 | 1.877 |
| Maximum | 0.199 | 0.558 | 0.832 | 343.50 | 0.591 | 1.994 | 1.121 | 2.553 |
| Mean | 0.172 | 0.36 | 0.64 | 159.40 | 0.415 | 1.378 | 0.745 | 2.184 |
| Std Deviation | 0.021 | 0.128 | 0.123 | 70.051 | 0.096 | 0.363 | 0.207 | 0.232 |
Control | | 0.05 | 0.12 | 0.30 | 118 | 0.25 | 0.88 | 0.29 | 1.30 |
Sub soil | Minimum | 0.102 | 0.123 | 0.315 | 114.80 | 0.258 | 0.885 | 0.395 | 1.158 |
| Maximum | 0.163 | 0.462 | 0.595 | 253.10 | 0.522 | 1.518 | 1.005 | 2.112 |
| Mean | 0.139 | 0.274 | 0.462 | 138.90 | 0.349 | 1.144 | 0.586 | 1.793 |
| Std Deviation | 0.021 | 0.125 | 0.103 | 43.791 | 0.088 | 0.235 | 0.197 | 0.314 |
Control | | 0.03 | 0.12 | 0.30 | 118 | 0.35 | 0.88 | 0.30 | 1.30 |
| WHO (1996) | 0.8 | | 36 | 30,000 | 85 | 2000 | 35 | 50 |
3.2 Spatial Distribution of the heavy metals in the soil
Cadmium spatial distribution
Figures 3a and 3b show the Cd distribution pattern in the soil. The variation map (Fig. 3a) shows that the degree of topsoil Cd concentration at the central part of the study area, opposed the concentration at north eastern part of the area. The highest Topsoil Cd concentration was observed at the North-eastern part of the community, while the lowest topsoil Cd level was recorded at the South-Western and North-central parts of the studied region. It was noted in the variation map that the northern part of the community tends to have higher Cd accumulation than the southern region of the community. This was contrary to the spatial distribution of Cd concentration in the subsoil. As shown in Fig. 3b, the northern region of the study area tends to have higher Cd accumulation, than the southern part of the community. Also, Fig. 3b revealed that the central part of the studied region experiences both high and low accumulation of Cd in the subsoil. It was also noted that the North-western part of the region, had moderate level of Cd concentration, which is similar to the topsoil Cd concentration level in the North-western part of the region.
Chromium spatial distribution
The spatial distribution of Cr in the topsoil and subsoil are presented in Figs. 4a and 4b. In Fig. 4b, topsoil Cr concentration increased non-evenly from the central part of the area to the boundaries of the area. The maximum topsoil Cr concentration was detected at the north eastern part of the area. Regarding the subsoil, the degree of accumulation of Cr, declined non-linearly from the eastern part to the western part of the area. Figure 4b depicted that the lowest subsoil Cr accumulation (0.224 mg/kg) was witnessed at the south-western part of the study area; while the north-eastern and south-eastern parts of the area recorded the maximum Cr concentration of 0.558 mg/kg. It was observed from the maps that the topsoil Cr distribution is similar to Cd topsoil distribution, which portrayed that both metals pollution might emitted from the same source.
Copper spatial distribution
Figures 5a and 5b revealed the spatial variation map of Cu accumulation level in the topsoil and subsoil. The topsoil (Fig. 5a) had bimodal Cu concentration – one maximum point located at the south-eastern part and the other located at the north eastern part of the area. Generally, the topsoil Cu concentration declined non-uniformly from the north-eastern part of the studied area to the south-western part if the studied region. Furthermore, the map depicted that the north-western and south-south parts of the studied region had average Cu topsoil concentration.
Regarding the subsoil (Fig. 5b), the map revealed that the highest Cu accumulation (0.595 mg/kg) was recorded at the north-central part of the area, while the lowest Cu accumulation was observed at the far north-eastern and the middle of the south-western parts of the community. Remarkably, most of the community’s subsoil has moderate Cu accumulation. The lower Cu concentration recorded at the edges of the community, could be linked to the remediation effects of the grasses growing in these parts. According to Chibuike and Obiora (2014), plants and decomposing organic materials have the ability of degrading the metals concentration in the environment (soil, air and water); hence, greatly assisting in clearing the contaminated ecosystems, and replenish the soil biochemical properties.
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Iron spatial variation The spatial of Fe concentration distribution in the community’s top sand sub soils are presented in Figs. 6a and 6b. The topsoil Fe variation map reveals that Fe was heavily concentrated (343.50 mg/kg) in northern part topsoil, while central part of the community recorded the least Fe concentration of 121.60 mg/kg. Figure 6a portrayed that the top soil Fe concentration declined non-linearly from the northern part of the community to the southern part of the community; though the north central part had overlapping Fe concentration. Similar to the topsoil Fe distribution pattern, the subsoil Fe concentration variation (Fig. 5b) revealed that the maximum Fe concentration was recorded at the north-eastern part of the area, while the lowest subsoil Fe content (114.80 mg/kg) was noted at the north central part of the studied area. This shows that the Fe level in the subsoil increased in a non-uniform pattern from the central part of the area to the boundaries.
Lead spatial distribution
The spatial distribution maps of Pb accumulation in the top and sub soils are presented in Figs. 7a and 7b. Figure 7a shows that Pb was visibly present in high concentration in the topsoil at the central part of the study area; while the community north-eastern part topsoil had the highest Pb concentration. The distribution of Pb across the community topsoil is similar to the pattern followed by Fe, when the concentration of the heavy metal increased non-linearly from the central to the edges of the area investigated in this research. Regarding the Pb concentration distribution in the subsoil (Fig. 7b), it was noted the variation followed similar trend as the topsoil Fe distribution. The lowest subsoil Pb content appeared at the north-central part of the area, which increased uniformly to the edges of the studied region.
Manganese spatial variation
The spatial variation of Mn concentration level in the topsoil and subsoil is presented in Figs. 8a and 8b. It was noted that the topsoil Mn concentration widely across the area (Fig. 8a); but the concentration generally decreased non-linearly from the southern part of the studied area to the northern part of the area investigated. The maximum and minimum Mn concentration was both recorded at the central part of the area. Apart from the central part of the investigated area, high accumulation of Mn was recoded in two other locations – one at the far north eastern part of the area, and the point was located at the south western part of the area. Likewise, the subsoil (Fig. 8b) Mn concentration distribution pattern was similar the variation observed in the topsoil. The Mn concentration was scanty in the northern region subsoil, while the south-eastern region of the area recorded high Mn accumulation.
Nickel spatial distribution
The spatial distribution map of Ni concentration in the top and sub soils are presented in Figs. 9a and 9b. As portrayed by the results, the highest Ni content in the top and sub soils was at the south eastern part of the study area. It was observed that large proportion of the topsoil has fairly high Ni concentration; whereas as the soil depth increases to 50 cm, the concentration of this region declined considerably. Traces of Ni were present in the soil in considerable amount at the middle part of the study area, irrespective of the sampling location.
Zinc distribution
The distribution maps (Figs. 10a and 10b) revealed that the topsoil Zn concentration varied widely from the central part of the study area to the edges of the area. Interestingly, maximum and minimum Zn concentration was detected at two spots in the topsoil, which is unique from the subsoil. Furthermore, Fig. 10b revealed the study area was largely covered with moderate Zn concentration. Similar results were reported by Ipeaiyeda and Dawodu (2008), where the Zn concentration around the auto-mechanic workshops varied widely, as the soil profile depth increased from 0 cm to 50 cm.
Similar patterns of uneven distribution of soil metals concentration were observed by Atikpo and Ihimekpen (2018) and Uguru et al. (2021) for other geographical regions. In contrast, the heavy metals concentration recorded in this study were far lower than the Pb concentration level obtained by the previous authors (Uguru et al., 2021; Atikpo and Ihimekpen, 2018). The uneven variation observed among the eight metals investigated in this research, can be linked to remediation effect, the soil moisture content, pH and organic materials content (Rakesh et al., 2013).
3.3 Evaluation of the soil quality
The Heavy Metals Contamination Factor
The results of the heavy metals contamination factor are given in Table 2. As shown in Table 2, Cd recorded the highest CF values both in the topsoil and subsoil; while Fe and Pb had the lowest CF value in the topsoil and subsoil respectively. It was detected that the heavy metals follows this pattern of contamination Fe < Mn < Pb < Zn < Cu < Ni < Cr < Cd in the topsoil; while in the subsoil the CF followed this inclining trend Pb < Fe < Mn < Zn < Cu < Ni < Cr < Cd. Judging the pollution of the area’s soil based on the CF, the topsoil had moderate contamination of Cu, Fe, Pb, Mn, Ni and Zn, and considerable contamination of Cd and Cr. Then the subsoil had moderate pollution degree of Cr, Cu, Fe, Pb, Mn, Ni and Zn, and considerable pollution degree of Cd. Generally, it was noted that CF of the metals declined with increase in the soil profile; this is an indication that the subsoil is less contaminated than the topsoil. This is similar to the observations of Darma et al. (2022), during an investigation of the effect of gold mines leachates on the soil mass; when the pollution degree declined significantly with an increase in the soil depth.
Table 2
The heavy metals contamination factor
| Cd | Cr | Cu | Fe | Pb | Mn | Ni | Zn |
Topsoil | 3.44 | 3.00 | 2.13 | 1.35 | 1.66 | 1.57 | 2.57 | 1.68 |
Subsoil | 4.63 | 2.28 | 1.54 | 1.18 | 1.00 | 1.30 | 1.95 | 1.38 |
Single pollution index
The individual pollution levels of the heavy metals among the 10 studied points are presented in Tables 3 and 4. The maximum topsoil cadmium SPI value (0.249) was located at Location C, while the lowest topsoil cadmium SPI result (0.18) was recorded at Location B. It was observed that the Cd pollution at all the sampling points was at moderate degree of pollution. Regarding the subsoil, the maximum SPI was located at Location D and the minimum SPI was observed in spatial Point B. The SPI results revealed that regardless of the sampling location, the Cd pollution at the topsoil and subsoil was at the safety level of pollution. Regarding the Cr pollution, the maximum topsoil chromium SPI value was located at Point C, while Point E had the lowest SPI value. The study findings revealed that Cr pollution at Points A, C, D and G had moderate level of Cr contamination; while Points B, E, F. H and I topsoil had mild degree of Cr pollution. With respect to the subsoil, the highest Cr SPI vale waste recorded at Point D; while Point A recorded the lowest Cr SPI value. In terms of the subsoil Cr pollution level, it can being seen form the findings (Fig. 4) that Locations C, D and G had moderate degree of Cr pollution; Locations F and H had mild level of Cr pollution; and Locations A, B, E and I had slight degree of Cr soil pollution.
Regarding the Copper pollution, the SPI values depicted that at the topsoil, the maximum and minimum SPI values were located at Points G and D respectively; while in the subsoil, the highest and lowest SFI values were detected at Locations I and H respectively. Additionally, the SPI results portrayed that Cu contamination of the area was at the safety pollution degree. It was observed that the iron SPI values was evenly distributed both in the topsoil and subsoil (the values lies between 0.004 and 0.005) across the study area, apart from Location I that recorded very high SFI values in the top and sub soil. From Tables 4 and 5, it can be realized that Fe pollution of the area topsoil and subsoil was within the safety pollution level. Similarly, the SFI values for Pb revealed that Location B had the highest pollution degree both in the topsoil and subsoil. It was also noted from the results that Pb pollution level in the soil (both top and subsoil) was at the safety pollution degree. The topsoil Mn and nickel SFI values ranged from 0.0005 to 0.001 and 0.0177 to 0.0263 respectively; and the SFI values recorded in the subsoil Mn and Ni pollution varied from 0.0004 to 0.0007 and 0.0113 to 0.0287 respectively. This is an indication that the Mn and Ni pollution level in the study area soil was within the safety degree of pollution. In addition, in the topsoil, the highest zinc SPI value (0.0511) was located at spatial Point D, and Location G had the minimum topsoil Zn SPI value of 0.0375. In the subsoil, the maximum and minimum Zn SFI values were 0.0422 at Point D and 0.232 at Point A. The range of SFI values obtain for Zn revealed that, the area had safety level of Zn pollution.
Table 3
Metal | Point A | Point B | Point C | Point D | Point E | Point F | Point G | Point H | Point I |
Cd | 0.243 | 0.191 | 0.249 | 0.233 | 0.191 | 0.18 | 0.241 | 0.206 | 0.198 |
Cr | 3.775 | 1.925 | 4.650 | 4.300 | 1.875 | 2.600 | 3.383 | 2.642 | 1.867 |
Cu | 0.017 | 0.016 | 0.019 | 0.02 | 0.015 | 0.016 | 0.023 | 0.012 | 0.022 |
Fe | 0.0043 | 0.0051 | 0.0050 | 0.0050 | 0.0041 | 0.0042 | 0.0044 | 0.0043 | 0.0115 |
Pb | 0.0064 | 0.0070 | 0.0051 | 0.0037 | 0.0037 | 0.0048 | 0.0042 | 0.0042 | 0.0049 |
Mn | 0.0006 | 0.0008 | 0.0005 | 0.0009 | 0.0006 | 0.001 | 0.0005 | 0.0007 | 0.0005 |
Ni | 0.0263 | 0.0127 | 0.0177 | 0.0225 | 0.0232 | 0.032 | 0.0178 | 0.0157 | 0.0235 |
Zn | 0.0409 | 0.0438 | 0.0446 | 0.0511 | 0.0423 | 0.0397 | 0.0375 | 0.0509 | 0.0423 |
Table 4
Metal | Point A | Point B | Point C | Point D | Point E | Point F | Point G | Point H | Point I |
Cd | 0.179 | 0.128 | 0.185 | 0.204 | 0.18 | 0.153 | 0.189 | 0.199 | 0.144 |
Cr | 1.025 | 1.617 | 3.625 | 3.850 | 1.208 | 2.350 | 3.075 | 2.258 | 1.525 |
Cu | 0.011 | 0.009 | 0.013 | 0.016 | 0.012 | 0.012 | 0.017 | 0.009 | 0.016 |
Fe | 0.0040 | 0.0046 | 0.0046 | 0.0044 | 0.0039 | 0.0039 | 0.0040 | 0.0038 | 0.0084 |
Pb | 0.0050 | 0.0061 | 0.0049 | 0.0031 | 0.0030 | 0.0042 | 0.0034 | 0.0036 | 0.0037 |
Mn | 0.0006 | 0.0006 | 0.0005 | 0.0007 | 0.0005 | 0.0008 | 0.0004 | 0.0006 | 0.0005 |
Ni | 0.0229 | 0.0117 | 0.0151 | 0.0147 | 0.0151 | 0.0287 | 0.0141 | 0.0113 | 0.0171 |
Zn | 0.0232 | 0.0381 | 0.0407 | 0.0422 | 0.0359 | 0.0312 | 0.0316 | 0.0422 | 0.0377 |
Pollution load index (PLI)
The soil heavy metals PLI results are presented in Table 5. It was revealed in Table 5 that irrespective of the sampling depth, Mn had the lowest PLI value while Cr had the highest PLI value. The topsoil PLI followed this increasing pattern Mn < Pb < Fe < Cu < Ni < Zn < Cd < Cr; while the subsoil PLI took this increasing trend Mn < Pb < Fe < Cu < Ni < Zn < Cd < Cr. Based on the pollution level of the toxic elements in the soil, the PLI values depicted that there was low level of Mn, Pb, Fe, Cu, Ni, Zn and Cd pollution in the soil; while Cr contamination was at moderate degree of pollution. Continued accumulation of heavy metals in the soil can result in greater toxic metals uptake by plants, and contamination of the water bodies. This may significantly increase the menaces, associated with heavy metals poisoning in the affected regions (Darma et al. 2022).
Table 5
Pollution load index values for soil
Metal | Top Soil | Subsoil |
Cd | 0.213 | 0.172 |
Cr | 2.835 | 2.069 |
Cu | 0.018 | 0.012 |
Fe | 0.005 | 0.004 |
Pb | 0.005 | 0.004 |
Mn | 0.001 | 0.001 |
Ni | 0.021 | 0.016 |
Zn | 0.043 | 0.035 |