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Groundwater recharge is the process by which water moves downward through the soil and rock layers to replenish aquifers. Aquifers are underground rock layers that hold and release water, serving as crucial sources of fresh water on Earth.12

Recharge occurs most effectively when rainfall exceeds water loss through evaporation and transpiration. If the water table is deep, aquifer water can be ancient, originating from past climates. This is known as groundwater mining when the water is used without sufficient replenishment, as seen in the Ogallala Aquifer.13

Over-extraction of groundwater can lead to falling water tables, increased pumping costs, and saltwater intrusion into coastal aquifers. Efforts to augment recharge include using wastewater and managing river flows.23

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