[[1]] act as a natural absorber of rainwater and allows it to seep. It helps maintain the water table throughout the year. 

Soil acts as a natural absorber of rainwater and allows it to seep into the ground.

When rainwater falls onto the soil, it can either be absorbed into the soil or run off the surface. The amount of water that is absorbed by the soil depends on the type of soil, its composition, and its ability to hold water. Soils with high organic matter content, such as those found in forests or grasslands, are better at absorbing water than soils with low organic matter content, such as those found in deserts or urban areas.

As rainwater seeps into the soil, it is filtered and purified, as the soil acts as a natural filter, removing impurities and pollutants. This filtered water eventually makes its way to underground aquifers, where it is stored until it is pumped out for human use.

In addition to absorbing and filtering rainwater, soil also helps to prevent erosion and flooding. Vegetation growing in the soil, such as trees and grasses, can help to hold the soil in place and slow down the movement of water across the landscape, reducing the risk of erosion and flooding.