Abstract

An assessment was carried out of the anthropogenic enrichment of the chemical composition of the bottom sediments of water bodies situated in an area with an urban and industrial character (63.7% of the total area). The endorheic catchments of the water bodies studied are lithologically uniform with sandy formations accounting for more than 90% of the surface area. On the basis of geoaccumulation index values, it was found that the bottom sediments of the water bodies studied were contaminated with the following elements: Cd, Zn, S, As, Pb, Sr, Co, Cr, Cu, Ba, Ni, V, Be, in degrees ranging from moderate to extreme, with lower contamination (or absence of contamination) with the same elements being found in the formations present in the vicinity and in the substrate of the basins of water bodies. It was found that one consequence of the fact that these water bodies are located in urban and industrial areas is that there is anthropogenic enrichment of the chemical composition of bottom sediments with certain basic components (organic matter, Mn, Ca and P compounds) and trace elements: Cd, Zn, Pb, Sb, As, Cu and Co, Br, Ni, S, Be, Cs, Sr, V, Cr, Sc, Ba, U, Ce, Eu and Th, with virtually no enrichment of sediments with the other basic and trace components analysed (La, Rb, K2O, Nd, Sm, Na2O, Hf, SiO2, Zr).

Highlights

  • The basins of water bodies serve as sedimentary basins and the sediments within them record the phenomena and processes occurring in the environment[1,2]

  • Field research covered a group of several water bodies in southern Poland (Fig. 1). These are located in the central part of the Silesian Upland on the boundaries of three cities: Katowice, Sosnowiec and Mysłowice

  • Variations in the chemical composition of sediments between individual endorheic water bodies are conditioned by the geological substrate, the manner in which the catchment is utilised and the type of atmospheric deposition[9]

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Summary

Introduction

The basins of water bodies serve as sedimentary basins and the sediments within them record the phenomena and processes occurring in the environment[1,2]. Since they constitute polygenetic material, the chemical composition of bottom sediments is largely dependent on natural conditions and human pressure[3,4,5,6,7]. A relatively new geoecological approach is an attempt to assess the degree of anthropogenic enrichment of the chemical composition of sediments against the background geochemical characteristics of the surface formations representative of the substrate and the area in the vicinity of water bodies[8]. Such geochemical testing of sediments is important in the case of water bodies that have a variety of economic uses, especially in densely populated areas where there is usually a shortage of water that is conventionally considered clean

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