groundwater

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Groundwater
Groundwater is water located beneath the ground surface in soil pore spaces and in the fractures of lithologic formations. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become fully saturated with water is called the water table. Groundwater is recharged from, and eventually flows to, the surface naturally; natural discharge often occurs at springs and seeps, streams and can form oases or wetlands. Groundwater is also often withdrawn for agriculturalmunicipal and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology, also called groundwater hydrology.
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Eau souterraine
L'eau souterraine désigne toutes les eaux se trouvant sous la surface du sol dans la zone de saturation et en contact direct avec le sol ou le sous-sol.
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Grundwasser
Grundwasser ist das Wasser, das unter der Erdoberfläche in Hohlräumen einen Wasserkörper bildet.
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Woda gruntowa
Woda gruntowa to zasoby wody w podziemnych warstwach skał, zwanych warstwą wodonośną. Jest ona zasilana przez wody opadowe, które przenikają przez warstwy przepuszczalne dla wody i zatrzymują się ponad warstwami nieprzepuszczalnymi. Jednak jej gromadzenie i magazynowanie wymaga dziesiątków lub setek lat. Z tego względu szybkie wykorzystanie, spowoduje jej niedobory (powolna regeneracja).
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Falda acquifera
Per falda acquifera (o falda idrica, secondo una vecchia definizione) s'intende l'acqua che circola nel sottosuolo. Grazie alle precipitazioni, si formano depositi di acque sotterranee che scorrono su un sottosuolo in quantità e con modalità che dipendono da fattori climatici, biologici e dalla permeabilità e inclinazione del terreno.
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