In the diploma thesis, we described the course of implementation and processing of permeability tests that were carried out as part of the expansion of the Ljubljana Railway Station and the construction of the Emonika commercial-residential complex. Drill-holes ZP-5-HG and V-EM-1-PT, where the tests were conducted, are located in the area where Masarykova ulica and trg Osvobodilne Fronte in Ljubljana intersect. Drill-hole ZP-5-HG was drilled to a depth of 15.8 meters, while V-EM-1-PT reached a depth of 16 meters. During drilling, we did not reach the bedrock of the Permian Carboniferous layers. The groundwater depth in the area of the railway station and the future Emonika complex ranges from 21.60 to 22.50 m below the surface. Both drill-holes are located entirely in Quaternary sediments of the highly permeable aquifer of the Ljubljana Basin, which is of great importance fort he drinking water supply of the Ljubljana city. The general groundwater flow is from northwest to southeast, with a significant inflow occurring through the Ljubljana Gate (the passage between Rožnik and Grad hill) from the south to the north. The estimated flow through the gate is approximately 500 liters per second.
Nonstationary permeability tests were conducted and processed using the Hvorslev method, which is based on analyzing the water level drawdown curve in the drill-hole. In drilll-hole ZP-5-HG, the average hydraulic conductivity was determined to be 1.16×10-3 m/s, with a range of coefficients ranging from 6.15×10 4 to 2.14×10-3 m/s. In drill-hole V-EM-1-PT, the average permeability coefficient was determined to be 1.10×10-3 m/s, with a range of coefficients ranging from 1.98×10-4 to 2.10×10-3 m/s.
Based on the hydrogeological classification, the area of Masarykova ulica in Ljubljana can be defined as highly permeable.
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