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Naslov:Multivariate statistical methods in determining the spatial distribution of chemical elements in soil from the Mavrovo-Rostuše region, North Macedonia
Avtorji:ID Stafilov, Trajče (Avtor)
ID Šajn, Robert (Avtor)
ID Petrovska, Kristina (Avtor)
Datoteke:.pdf PDF - Predstavitvena datoteka, prenos (1,90 MB)
MD5: 6930597327468D5F40AC7E5117DF0386
 
Jezik:Angleški jezik
Tipologija:1.01 - Izvirni znanstveni članek
Organizacija:Logo GeoZS - Geološki zavod Slovenije
Povzetek:In this work, the contents and spatial distributions of 19 elements (Ag, Al, B, Ba, Ca, Cr, Cu, Fe, K, Li, Mg, Mn, Na, Ni, P, Pb, Sr, V, Zn) in the soil of the western part of North Macedonia (Mavrovo-Rostuše region) are presented. For this purpose, a total of 66 soil samples were collected from 33 locations (33 samples of topsoil, 0-5 cm, and 33 samples of subsoil, 20-30 cm). All samples were analysed by inductively coupled plasma - atomic emission spectrometry (ICP-AES) after complete digestion with four acids (HNO3, HF, HClO4 and HCl). The obtained results were statistically evaluated and spatial distribution maps for all analysed elements were also prepared. Factor analysis was performed to reduce the number of data used and new synthetic variables (factors) were identified. Through the application of factor analysis, three geochemical associations were identified: Factor 1 (Zn, K, Cu, Fe, and Li), Factor 2 (Cr, Ni, and Mg) and Factor 3 (Ca and Al). From the obtained data and the maps of spatial distribution, it could be concluded that the distribution of the analysed elements is related to the lithology of the region. Thus, it was found that the higher content of elements of Factor 1 occurs in the eastern and southern part of the study area (middle and lower reaches of the Radika River and along the Mala River), where Mesozoic and Paleozoic carbonates as well as Paleozoic shales and Paleogene flysch prevail. Factor 2 (Cr, Ni and Mg) also represents a lithogenic association. The highest contents of the elements in both soil layers were found in the areas where Paleozoic sandstones and shales (village of Lazaropole and the area around the Mavrovo Lake) and Paleogene flysch (Rostuše village) predominate. Factor 3 (Ca and Al) also represents lithogenic association of elements. The highest content of these elements was found in the northwestern part of the study area (village of Žirovnica and along the Berička River) and in the northeastern region above the village of Brodec where Mesozoic carbonates and Paleogene flysch dominate.
Ključne besede:soil, heavy metals, spatial distribution, Mavrovo-Rostuše region, North Macedonia
Status publikacije:Objavljeno
Verzija publikacije:Objavljena publikacija
Datum objave:30.12.2023
Založnik:Macedonian Ecological Society
Leto izida:2023
Št. strani:str. 75-91
Številčenje:vol. 25, no. 2
PID:20.500.12556/DiRROS-17631 Novo okno
UDK:504.5
ISSN pri članku:1857-8330
DOI:10.59194/MJEE23252075s Novo okno
COBISS.SI-ID:179189763 Novo okno
Datum objave v DiRROS:04.01.2024
Število ogledov:605
Število prenosov:174
Metapodatki:XML DC-XML DC-RDF
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Gradivo je del revije

Naslov:Macedonian journal of ecology and environment
Založnik:Macedonian Ecological Society
ISSN:1857-8330
COBISS.SI-ID:2369109 Novo okno

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Licenca:CC BY 4.0, Creative Commons Priznanje avtorstva 4.0 Mednarodna
Povezava:http://creativecommons.org/licenses/by/4.0/deed.sl
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