how does nature maintain groundwater reservoirs ?
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The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called thewater table. Groundwater is recharged from, and eventually flows to, the surface naturally; natural discharge often occurs at springs andseeps, and can form oases or wetlands.
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- When precipitation falls, the water percolates into the rock layer of the ground and then through flow occurs, leading the water back to underground reservoirs. ...
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