ANTHROPOGENIC CONTAMINATION DEGREE OF GROUNDWATER WITHIN NORTHERN PART OF TUREK GLACIAL UPLAND
Journal Title: Biuletyn Państwowego Instytutu Geologicznego - Year 2011, Vol 445, Issue 445
Abstract
The objective of this study was to identify the influence of the brown coal mine anthropopresion on chemical composition of groundwater in the Quaternary aquifer and in the Upper Cretaceous aquifer in Turek Glacial Upland. Generally, the water chemistry within Upper Cretaceous aquifer is controlled by natural processes, whereas in the Quaternary aquifer antropogenic influence can be seen.
Authors and Affiliations
Dorota POROWSKA, Katarzyna SAWICKA
Keywords
Related Articles
- EP ID EP64069
- DOI -
- Views 61
- Downloads 0
ZAŁOŻENIA TEKTONICZNE I GENEZA OKNA TEKTONICZNEGO SMILNA (WSCHODNIA SŁOWACJA)
Tektoniczne okno Smilna położone jest na obszarze wschodniej Słowacji, w obrębie jednostki magurskiej. W obrębie okna Smilna mamy do czynienia z profilami dwóch jednostek, jednostki dukielskiej i jednostki grybowskiej. O...
GEODYNAMICS OF THE SELECTED AREAS IN POLAND ON THE BASIS OF THE SATELLITE RADAR INTERFEROMETRY
Three areas on the territory of Poland were selected as the test sites. They were characterized by different landscape, geological setting and land use. They cover southern coasts of the Baltic Sea around Gdańsk Bay, fra...
Mesozoic spores of Poland – a revision of selected taxa
The study presents a taxonomic analysis of 44 taxa from the Mesozoic deposits of Poland. The spores have been ordered in a systematic way. Variability in interpretations of similar morphological or typical features of in...
GEOLOGICAL CONDITIONS OF MUNICIPAL WASTE LANDFILLING
Not sealed landfills provide one of the most dangerous threats for ecosystems, and for health and existence of people. High production of wastes, and big diversity of their compositions are inherent in the human developm...
Osady paleogenu i neogenu w wielkoskalowych strukturach glacitektonicznych Wzgórz Dylewskich
Badawczy otwór wiertniczy w Wysokiej Wsi, zlokalizowany w centrum Wzgórz Dylewskich (NE Polska), osiągnął głębokość prawie 490 m, z czego na ponad 400 m przewiercono utwory paleogenu i neogenu. W wyniku badań palinologic...