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EN
Two geophysical field works were conducted during a feasibility study in the Smaltjärnen tailing repository of the abandoned Yxsjöberg mine, located in south-central Sweden. The aim of these studies was to evaluate the applicability of the geophysical methods in tailing characterizations i.e. to (I) identify the approximate level of the underground water table, (II) understand the vertical and lateral distribution of the tailings and (III) image the variations within the internal stratigraphy of the tailings. Ground Penetrating Radar (GPR) data with medium–low-frequency antennas (300, 250 and 100 MHz) and Self-Potential (SP) data using the Streaming Potential Phenomena (SPP) were collected to characterize the top few meters of the subsurface and understand the water flow direction. Results from the mineralogical and geochemical studies of the drill-core samples were incorporated in the study to complement the interpretations of the geophysical data. Three distinct layers had been earlier identified based on the interpretations of the geochemical data which agreed well with the GPR interpretations in this study: (I) oxidized tailing (new), (II), transition zone and (III) old tailing which is located under the water table. The SP data, unexpectedly, indicated that the groundwater flows from the lake i.e. lower altitudes, towards the higher altitudes which probably is related to the uncertainties resulted from 2D data while the actual water flow direction can be best studied in 3D, or, dominant effect from the metal contents. Complementary geophysical studies including a 2D-SP survey and Direct Current (DC) electrical resistivity measurements are suggested to improve the present understanding of the morphology of the site.
EN
The Ruczaj district in Kraków is the potential building area of high flat blocks for inhabitants. This area is built of the gypsum basement covered by the soil and impermeable clay beds with several meters of thickness. The flat blocks must be set on the textured gypsum layer. In the result of the rainfall and static pressure of the blocks, the water with SO42− increases up to the groundwater level, become the great threat for the flat blocks. The water creates specific hydrogeological conditions occurring in the zone of the building’s foundations. To eliminate the mentioned threat, we should determine precisely the thickness of the soil and impermeable clay as well as the depth of the gypsum basement. Based on the electromagnetic parameters of the geological formations, the Ground Conductivity Meter and DC resistivity methods were used to solve the mentioned problems.
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