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Groundwater recharge
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Groundwater that recharges an aquifer
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Wikipedia

Groundwater recharge or deep drainage or deep percolation is a hydrologic process, where water moves downward from surface water to groundwater. Recharge is the primary method through which water enters an aquifer. This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table surface....

Instance of
Hydrology
References
Wikidata