The analysis of river and lake sediments indicates that the physical, chemical, biochemical and geochemical
processes that influence the fate of toxic compounds and elements in sediments are numerous and complex
(for example: sorption - desorption, oxidation - reduction, ion-exchange, biological activity). Due to the
above-mentioned general statement, only a long term and complex research programme can lead to satisfactory
answers to the questions relating to possible changes of water and environmental quality in the future.
The aim of our study consisted in physical and chemical characterisation of sediments in in-depth profiles
taken from the Dobczyce reservoir in southern Poland that is a main source of drinking water for the city
of Kraków. Due to morphological reasons, 7 layers of sediment samples were distinguished from the ground
level to about 90 cm below (total thickness of the sediments in the sampling site). Analysis of grain size distribution
and application of x-ray diffraction method, enabled mineralogical description of sediments.
The use of proton-induced x-ray emission (PIXE) and atomic absorption spectrometry (AAS) revealed
elemental composition of the samples (Al, P, K, Ca, Sc, Ti, V, Cr, Mn, Fe, Co, Ni, Cu, Zn). Concentrations
of natural 40K and artificial 137Cs radionuclides were determined by the use of gamma spectrometry.
The following facts were established: 1) the oldest (deepest) and newest, recently deposited layers of
sediments are similar in their physical and chemical properties. It means that the inflow of contaminants
and biogenic compounds to the reservoir has changed little since it was constructed and filled with water;
2) the severe flood in 1997 changed significantly sediment composition and, in fact, led to purification of
sediments in the Dobczyce reservoir
