Natural Groundwater Recharge Process
Groundwater recharge mainly occurs via natural processes. Rain soaks into the ground, rivers gradually seep into underground channels, and as snow slowly melts in springtime, it adds to groundwater reserves. These natural processes are essential, particularly in areas where the seasons bring significant changes in water availability. These natural processes are influenced by several key factors:
Soil Type: Sandy soils allow water to flow faster, whereas clay-rich soils slow it down.
Vegetation: Thick flora, supported by efficient forest cover, allows a greater amount of water to filter into the ground.
Climate: With average rainfall and more water flowing into rivers instead of evaporating, groundwater recharge improves.