What can slow surface runoff do to aquifers?

Slow surface runoff is beneficial for aquifers because it allows water to gradually infiltrate the ground, promoting the replenishment of these underground water reserves. When water flows slowly over the surface, it gives it more time to soak into the soil, which increases the likelihood of reaching the aquifers below. This process is essential for maintaining water levels in aquifers, especially during dry conditions or periods of low precipitation.

Additionally, increased infiltration contributes to the natural filtration of water, where the soil and other geological layers help remove impurities before the water reaches the aquifers. This replenishing effect is crucial for sustainable water supply management, particularly in regions that rely heavily on aquifers for drinking water and irrigation. Overall, the slow movement of surface runoff directly supports the health and sustainability of aquifers.