Explain the ground water is recharge
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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. Recharge occurs both naturally (through the water cycle) and through anthropogenic processes (i.e., "artificial groundwater recharge"), where rainwater and or reclaimed water is routed to the subsurface.
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Through the process of infiltration, the groundwater is refilled.
- Water travels downhill from surface water to groundwater during a hydrologic process known as groundwater recharge, deep drainage, or deep percolation.
- The primary way that water enters an aquifer is through recharge.
- Rainwater and water from other sources, such rivers and ponds, permeate the soil and fill crevices and gaps that are many feet underground.
- Infiltration is the term used to describe the process by which water seeps into the soil. Or also we can say that the Infiltration is the process by which water on the ground surface enters the soil. The infiltration process recharges groundwater.
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