The inflitration of water into the subsurface is the
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Infiltration is the process by which water on the ground surface enters the soil. It is commonly used in both hydrology and soil sciences.
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The infiltration of water into the subsurface is the recharge.
- From aboveground, the water flows into the subsurface in case of infiltration.
- The water seeps into the ground and the groundwater is replenished as a result.
- The rate of infiltration and its pattern depends on various factors such as the water table's depth, the subsurface materials' hydraulic properties, and the distribution of water at the ground surface.
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