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(groundwater regime, catchment area, real evapotranspiration, dynamic volume, water budget, Belo Vrelo, Serbia)
streams. In the case of fracture porosity,groundwater pathways are determined by the geological formation, extent of fracturing and local hydrogeological conditions. At Belo Vrelo, groundwater circulates within faults, fractures

the hydrogeological characteristics of the area, the qualitative andquantitative characteristics of the groundwater, andthe variations in these parameters over time. Theaquifer regime is governed by a series of factors,

of transformation of precipitation into a discharge hydrograph. It isalso possible to determine dynamic groundwater volumes in a karst spring catchment area, the water budgetequation parameters and the like. It should be