Abstract

Common occurrence of copper and zinc in groundwater and their diverse mobility in the environment make these metals sensitive indicators of industrial and municipal pollution of freshwaters. An analysis of the collected data allowed for a description of the factors and processes that induce changes in the concentration of these metals in the soil, rock and groundwater. Sorption, ion exchange and oxidation–reduction processes, dissolution and precipitation of minerals, and reactions involving organic matter significantly affected the mobility of copper and zinc. The study employed hydrogeochemical methods to obtain comprehensive interpretative data. Its results showed that the variability of the composition of exchangeable cations was due to instability of chemical composition of precipitation. Different activities of Cu and Zn in the solution introduced into the rocks led to the establishment of new quasi-equilibrium states between the adsorbent and the adsorbate. At very low copper and zinc concentrations in groundwater, zinc was more easily retained in the solid phase, and it was more difficult to extract. In contrast, a laboratory static batch experiment utilizing high concentrations of the elements in the solutions showed their different behavior. The sorption of copper occurred more easily than the sorption of zinc, as evidenced by the study results and the calculated parameters of sorption maximum, binding constant, and degree of surface coverage of the solid phase by adsorbed copper and zinc according to a single Langmuir equation.

Highlights

  • Vadose zone is the zone of the most intense interactions between infiltrating rainwater, soil framework and gas phase in the rock pores

  • The sorption of copper occurred more than the sorption of zinc, as evidenced by the study results and the calculated parameters of sorption maximum, binding constant, and degree of surface coverage of the solid phase by adsorbed copper and zinc according to a single Langmuir equation

  • The amount of zinc and copper adsorbed by soil and rock components under equilibrium conditions depends basically on the content of organic matter, clay minerals and metal oxides and hydroxides (Stumm and Morgan 1981; Ross 1994; Arias et al 2005)

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Summary

Introduction

Vadose zone is the zone of the most intense interactions between infiltrating rainwater, soil framework and gas phase in the rock pores. Zinc and copper are elements that accurately document the effects of industrial and municipal pollution. Their widespread occurrence in groundwater and diverse mobility in the environment make these metals sensitive indicators of freshwater pollution. Zinc and copper are among water migrants with a high migration contrast. The mobility of zinc and copper depends on the properties of both the solid phase and the solution. In the weathering zone under oxidizing conditions, easy solubility of zinc sulfates facilitates an intense migration of this metal, which becomes one of the most mobile water migrants (Ajwa and Tabatabai 1997). A decrease in zinc activity is a result of both a formation of metallo-organic complexes and an increase in ionic strength of the solution (Diatta and Kociałkowski 1998)

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Results and discussion
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Conclusions
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