The utilization of aquifers beyond their flow and recharge capacities is known as

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Groundwater mining refers to the excessive use of groundwater from aquifers, leading to depletion and permanent damage to the water resources. It occurs when water withdrawals exceed the natural recharge rate, leading to a decline in the water table and reduced availability of groundwater. Potentiometric surface refers to the level to which water from an aquifer would rise under natural conditions. Contact surface refers to the interface between two different types of rock or soil layers. Influent conditions refer to the state in which water flows from the ground surface into the aquifer.

The Utilization of Aquifers Beyond Their Flow and Recharge Capacities