Abstract: More accurate interpretations are required in order to understand the processes of hydrological movement and hydrochemical variation of water flow in epikarst. A drip VP1 from the Velika Pasica Cave (Central Slovenia) was studied during a period which occurred at the end of a long wet, cold winter. The sources of the percolation water in the cave were both from rain water and snowmelt water. The discharge was continuously monitored during study period in one hour intervals. Each hour a water sample from the drip was taken for measurements of pH...
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