Nitrates in groundwater of the upper Liswarta River basin
Journal Title: Biuletyn Państwowego Instytutu Geologicznego - Year 2008, Vol 432, Issue 432
Abstract
The upper Liswarta River basin is situated in the drainage area of the Warta River. The chemical composition of groundwater in the investigated area is the result of natural and anthropogenic factors. Lithology of the aeration and saturation zones and the differentiation of oxidation-reduction conditions along the path of water circulation have the main influence on groundwater quality. The worsening quality of groundwater in the area of the upper Liswarta River basin is due to the influence of anthropogenic factors including the leaching migration of nitrates from surface contamination spots as a result of soil cultivation and fertilisation, animal farming and social-living activities within rural areas. An important factor influencing the water quality is hydrogeochemical changes in water consumption conditions.The assessments of groundwater chemistry and quality of the Quaternary aquifer within the upper Liswarta River basin were determined from the results of 74 chemical analyses. The study results indicate that groundwater in the area is represented by multi-ion fresh waters, slightly acid to slightly basic (pH values range from 5.35 to 9.56). The TDS of these waters reaches up to 672.35 mg/l, with average of 295.36 mg/l. The tested waters show the presence of increased concentrations of nitrates, sulfates, and sometimes chlorides, which are the indicators of anthropogenic contaminations. Nitrate concentrations in the groundwaters are up to 189.00 mg/l, and the content of sulfates ranges from 5.47 to 178.00 mg/l.The mosaic concentration distribution of nitrates in groundwater can suggest local contamination of single water intakes. The differentiated distribution of the nitrates concentration in some wells and observation boreholes, especially in rural area, is probably related the type of land use and land development.
Authors and Affiliations
Martyna GUZIK
FORECAST OF DEVELOPMENT OF DEPRESSION CONE AND WATER INFLOWS TO BROWN COAL MINE KONIN INCLUDING DESIGNED OPEN PITS TOMISŁAWICE AND OŚCISŁOWO
Hydrogeological model developed for KWB Konin covers approximately 2000 km2. This is the unsteady three-dimensional model of 5-layer, built using Visual Modflow. Model calibration was based on measurements of piezometric...
The standard section of Neogene deposits from Eastern Pomerania at Łęczyce near Lębork (Northern Poland)
The reported study focused on a complex analysis of Paleogene–Neogene section located at Łęczyce near Lębork (Eastern Pomerania). The lower part of the section is represented by Lower Oligocene to Miocene deposits, drill...
PROSPECTING FOR CONCEALED AND HIDDEN MINERAL DEPOSITS IN POLAND RESULTS AND POSSIBILITIES
Security of supply of mineral commodities is the basic concern of European Union. The present knowledge of geology makes low possibilities of discovery new deposits by grassroots prospecting. Prospecting of concealed and...
POTENCJAŁ ZASOBOWY WĘGLA BRUNATNEGO W POLSCE I MOŻLIWOŚCI JEGO WYKORZYSTANIA
Bardzo bogate zasoby węgla brunatnego w Polsce, formalnie przekraczające 37 Pt (łącznie zasoby udokumentowane i perspektywiczne), są faktycznie dostępne jedynie w niewielkiej części. Wynika to z istniejącego konfliktu z...
INTERACTION OF COAL MINING WASTES AND POWERPLANT COAL ASH AND ITS EFFECT ON THE PORE SOLUTION CHEMISTRY IN A DISPOSAL SITE
This study was aimed at elucidating the mode of interaction of coal mining waste and coal ash, exemplified in the Przezchlebie fly ash impoundment, where 12 years after closure, acidification of dewatered material and po...