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atBelgrade Groundwater Source. As a result, well discharge capacities vary over a broad range and groundwater levels in the capture zones differ even when the rate of discharge is the same. Five characteristic groundwater level

The groundwater surface in the capture zone ofwell RB-23 is typical of a high hydraulic conductivity aquifer: the impact of groundwater extractionspreads far beyond the capture zone of the laterals andthe groundwater surface

Geologic framework andhydrogeologic featuresBelgrade Groundwater Source (BGWS) is locatedalong the Sava River, in Quaternary fluvial sediments.The boundary of the groundwater source (protectionzones) encompasses, for the most