Infiltration is the process of rainwater soaking into the ground to replenish aquifers in the water cycle.
Infiltration is the process by which some rainwater seeps into the ground to replenish aquifers, which are saturated subsurface rock formations storing freshwater.
Groundwater recharge occurs through infiltration where water permeates through soil and enters aquifers, sustaining water supply.
Transpiration and evapotranspiration also play roles in the movement of water through the water cycle, contributing to replenishing groundwater sources.
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