Once rainwater is absorbed into the soil, it can follow several pathways:
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Infiltration: Some of the rainwater seeps down through the soil layers and recharges groundwater sources.
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Plant uptake: Plants absorb water from the soil through their roots for growth and photosynthesis.
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Runoff: If the soil becomes saturated or impermeable, excess water can flow over the surface as runoff, which may lead to erosion and water pollution.
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Groundwater flow: Water that infiltrates deep into the soil can flow laterally through underground aquifers, contributing to the replenishment of water sources such as wells and springs.
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Evaporation and transpiration: Some rainwater may evaporate back into the atmosphere or be released by plants through transpiration.
Overall, the absorption of rainwater into the soil plays a crucial role in maintaining ecosystem functions, supporting vegetation growth, and sustaining water resources.
