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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

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not considerably altered.The groundwater level at pieHydraulic characterization of laterals as applied to selected radial collector wells at Belgrade Groundwater Source 39Fig. 3. Groundwater levels in the zone of well RB-8m

require prior hydrodynamic analysis by simulating groundwater extraction conditions on anumerical model. The first step of the proposed approach is to assess the groundwater level regime formed inthe capture zone when the well

radial collector well, production causes the formation of a certain dynamic groundwater level in the zone of influence. The surface of the groundwater level in the capture zone is typically three-dimensional. Given thepresent