Geochemistry
Infiltration is the process by which water seeps into the soil from the surface, allowing it to percolate downward through the soil layers. This movement of water is crucial for replenishing groundwater supplies and plays a key role in the water cycle by ensuring that precipitation contributes to groundwater recharge rather than simply running off into surface water bodies. Understanding infiltration helps to manage water resources effectively and supports plant growth by providing essential moisture.
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