Trace metals concentrations in schoolyard and playground soils in Coronel city, Chile

Author(s):  
Pedro Tume ◽  
Viviana Acevedoa ◽  
Núria Roca ◽  
Jaume Bech

<p>An urban world population of 0.75 billion in 1950 and expected 6 billion in 2050 shows the tremendous potential growth of urban areas. The urban soil fulfills the role of the reactor for the physical, chemical and biological transformations of matter but also covers such functions as reduction of air pollution, regulation of climate elements in cities, source of biodiversity and formation of areas for ornamental and recreation purposes. As a usual part of urban ecosystems, urban soils in general have high concentrations of trace elements derive from human activities. The objectives of this work were (1) to quantify the concentrations and establish background levels of Ba, Co, Cr, Cu, Mn, Pb, Ni, V and Zn in soils of Coronel city; (2) to assess the degree of pollution and identify local sources of pollution and (3) to assess the health risks of TE in soils of Coronel city. From Coronel city were collected 129 samples from 43 sites located in schoolyards and playground areas. At each sampling point were taken three samples: topsoil sample (TS) (0-10 cm), subsoil sample (SS) (10-20 cm) and deep soil sample (DS) (150 cm). Multivariate statistical analysis and depth ratios were used to distinguish the source. Ecological indices were implemented to evaluate the degree of contamination. The median and (range) of the trace elements (TE) in TS were Ba 38 mg kg<sup>-1</sup> (12-147 mg kg<sup>-1</sup>), 38 mg kg<sup>-1</sup>; Co 4-40 mg kg<sup>-1</sup>; 15 mg kg<sup>-1</sup>; Cr 10-35 mg kg<sup>-1</sup>, 18 mg kg<sup>-1</sup>; Cu 12-70 mg kg<sup>-1</sup>, 22 mg kg<sup>-1</sup>; Mn 167-950 mg kg<sup>-1</sup>, 536 mg kg<sup>-1</sup>; Ni 11-115 mg kg<sup>-1</sup>, 35.5 mg kg<sup>-1</sup>; Pb 1.5-115 mg kg<sup>-1</sup>, 6 mg kg<sup>-1</sup>; V 52-528 mg kg<sup>-1</sup>, 94 mg kg<sup>-1</sup>; Zn 42-373 mg kg<sup>-1</sup>, 65 mg kg<sup>-1</sup>. Depth ratios and multivariate statistical analysis suggested that Co, Ni and Mn have principal contribution of geogenic sources and Ba, Cr, Cu, Pb, V and Zn anthropogenic sources. The upper limit of background values estimated with median absolute deviation (MAD) method and DS samples were Ba 30 mg kg<sup>-1</sup>,  Co 24 mg kg<sup>-1</sup>,  Cr 22 mg kg<sup>-1</sup>,  Cu 24 mg kg<sup>-1</sup>,  Mn 662 mg kg<sup>-1</sup>,  Ni 66 mg kg<sup>-1</sup>,  Pb 1.5 mg kg<sup>-1</sup>,  V 108 mg kg<sup>-1</sup>,  and Zn 52 mg kg<sup>-1</sup>. Contamination factor showed that some soil sample were categorized as considerable contamination to very high contamination for Pb, Zn and V. Both Hazard index and cancer risk indicated no adverse health effects.</p><p><strong>Keywords</strong>: Heavy metals, urban soils, ecological indices, health risk assessment</p>

2019 ◽  
Vol 12 (3) ◽  
pp. 199-212 ◽  
Author(s):  
Elena V. Shabanova ◽  
Ts. Byambasuren ◽  
G. Ochirbat ◽  
Irina E. Vasil'eva ◽  
B. Khuukhenkhuu ◽  
...  

This article focuses on the relationships between major (Si, Al, Mg, Fe, Ca, Na, K, S, P and Ti) and potentially toxic trace (Ag, As, B, Ba, Bi, Co, Cd, Cr, Cu, F, Ge, Mo, Mn, Li, Ni, Pb, Sb, Sn, Sr, Tl, V and Zn) elements in Ulaanbaatar surface soils and also sources of the trace elements in the soils distinguished by the methods of multivariate statistical analysis. Results of exploratory data analysis of 325 Ulaanbaatar soil samples show the accumulation of Ca, S, B, Bi, Cu, Mo, Pb, Sb, Sn, Sr and Zn in urban soils. The major elements were grouped by cluster analysis in tree associations characterizing main soil fractions: sandy P-(K-Na-Si), clayey (Mg-Ti-Fe-Al) and silty (S-Ca). The factor analysis shows that silty fraction is enriched in major elements of both natural and anthropogenic origin. The principal component analysis from 32 variables extracted nine principal components with 82.49% of the cumulative explained variance. The results of cluster and factor analyses well agree and reaffirm the enrichment causes of potentially toxic elements are a coal combustion at thermal power stations (B, Bi, Ca, Mo, S and Sr) and traffic emissions (Cu, Pb, Sn and Zn). Spatial distributions of trace elements in the districts of Ulaanbaatar city were obtained by ordinary kriging. It is illustrated that the different principal components define the various origins and patterns of accumulation of trace elements in soils. The supplementation of data set by the concentration of organic carbon and the species of elements could help to identify the sources of such elements as P, Ni, Al, Fe, Ca, Ba, Bi, Cr, Zn, Sr and Sb in urban soils more completely.


2001 ◽  
Vol 34 (3) ◽  
pp. 1255
Author(s):  
S. PANILAS ◽  
G. HATZIYANNIS

Multivariate statistical analysis was used on existing geochemical data of the Drama lignite deposit, eastern Macedonia, Greece. Factor analysis with varimax rotation technique was applied to study the distribution of major, trace and rare earth elements in the lignite and 850°C lignitic ash, to find a small set of factors that could explain most of the geochemical variability. The study showed that major elements AI, Na, Κ, contained in the lignite samples, presented high correlation with most of the trace and rare earth elements. In 850°C lignitic ashes major and trace elements present different redistribution. Only Al remained correlated with the trace elements Co, Cr, Rb, Ta, Th, Ti, Sc and rare earths related with inorganic matter in the lignite beds. Trace elements Fe, Mo, U, V, W, and Lu were associated with organic matter of lignite and had also been affected by the depositional environment.


2015 ◽  
Vol 68 (2) ◽  
pp. 147-159 ◽  
Author(s):  
Yousef Habous Nazzal ◽  
Nassir S. N. Al-Arifi ◽  
Muhammad Kamran Jafri ◽  
Hossam Kishawy ◽  
Habes A Ghrefat ◽  
...  

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