Influence of climate factors on soil heavy metal content in Slovenia

• Published in: Journal of soils and sediments Vol. 17; no. 4; pp. 1073 - 1083
• Main Author: Zupancic, Nina
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01.04.2017; Springer Nature B.V
• Subjects: Climate; Dolomite; Earth and Environmental Science; Environment; Environmental Physics; Geochemistry; Grasslands; Heavy metals; Leaching; Lithology; Sec 4 • Ecotoxicology • Research Article; Soil contaminants; Soil Science & Conservation; Soils; Spectrometry; Triassic; Variance analysis; Vegetation cover; Slovenia; MED, Adriatic Sea; MED, Slovenia; Enrichment by leaching; Eolian contribution; Dolomite; Analysis of variance; Climate factors
• ISSN: 1439-0108; 1614-7480
• DOI: 10.1007/s11368-016-1614-z

Purpose In spite of equal lithology, the local climate can affect soils’ geochemical characteristics. We investigated the dependence of heavy metal content on climatic factors according to a hierarchical nested analysis of variance design (ANOVA). Materials and methods We examined the heavy metal content in soils developed on the Upper Triassic dolomite at six locations situated at increasing distances from the Adriatic Sea towards inland. We tested the influence of the locations’ position, i.e. climate, vegetation cover, small-scale variability and analytical error. Co, Cr, Cu, Ni, Pb and Zn contents were determined by emission spectrometry. Results and discussion An initial increase in annual precipitation towards inland is followed by a steady decrease. Very high small-scale variability prevented statistically significant differences from being established at the location level due to the high variance components exhibited. However, the simpler one-way and non-parametric varieties of ANOVA confirmed significant differences in Co, Cr and Ni among locations. The differences are more pronounced in grassland soils where the Cu and Pb contents also differ between locations. There is a positive correlation among annual precipitation, Co, Cr and Ni, and it seems that the prevailing winds can also influence their content in soils. Conclusions The Co, Cr, Cu and Ni values are readily the highest in those locations with the greatest precipitation, possibly due to their resistance to leaching. The soils could be additionally enriched by an eolian contribution from the SW located outcropping flysch rocks. The established variability could be due to somewhat different dolomite composition. The reasons for the observed geochemical variability are complex and only partly due to climate.