The ground water budget analysis and the comparison between piezometric levels in the last twenty years in the Savone River basin (Roccamonfina Hydrogeological Unit), show that the ground water lowering is greater than what could be expected taking into account the consumptive use of water made in the area. S the intake area of the basin is larger than the constructed with the isopesti trend of the regional aquifer. Therefore the ground water recharge in the plain area is related to the deep water reservoir. It is possible that, in the last ten years, the strategic water reservoir us deduced from hydrostructural scheme are just developed
Capelli, G., Mazza, R., Trigari, S., Catalani, F. (2000). Le risorse idriche sotterranee strategiche nel distretto vulcanico di Roccamonfina (Campania nord-occidentale). QUADERNI DI GEOLOGIA APPLICATA, 2, 433-442.
Le risorse idriche sotterranee strategiche nel distretto vulcanico di Roccamonfina (Campania nord-occidentale)
CAPELLI, Giuseppe;
2000-01-01
Abstract
The ground water budget analysis and the comparison between piezometric levels in the last twenty years in the Savone River basin (Roccamonfina Hydrogeological Unit), show that the ground water lowering is greater than what could be expected taking into account the consumptive use of water made in the area. S the intake area of the basin is larger than the constructed with the isopesti trend of the regional aquifer. Therefore the ground water recharge in the plain area is related to the deep water reservoir. It is possible that, in the last ten years, the strategic water reservoir us deduced from hydrostructural scheme are just developedI documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
