ABSTRACT
Migration of metals/metalloids and their inorganic forms from bottom sediments into waters and from waters into bottom sediments is a complex process. Understanding this mechanism is essential for recognising transformations that occur in water reservoir ecosystems. The following research was conducted in 2012–2014. The aim was to define the time and spatial correlations in the changes of total and ionic antimony, arsenic and chromium concentrations in waters and bottom sediments of three water reservoirs located in Upper Silesia (Poland), i.e. Pławniowice, Rybnik and Goczałkowice. The ionic form contents were determined with high-performance liquid chromatography-inductively coupled plasma-mass spectrometry (HPLC-ICP-MS). The research was carried out to verify whether the bottom sediments deposited in the discussed reservoirs could have posed an environmental threat due to the possible release of toxic ionic forms (i.e. As(III), Sb(III) and Cr(VI)) into the pelagic zone. The comparison of the research results obtained for three reservoirs (being under different anthropopressure influence) enabled the researchers to describe the bioavailability of specific elements and their species. It also helped to discern the existing environmental threats for such water reservoirs and their users.
Disclosure statement
No potential conflict of interest was reported by the authors.