 Infiltration (hydrology)

Infiltration in hydrology refers to the process through which water on the ground surface enters the soil. This process is a critical component of the hydrological cycle and significantly influences soil moisture, groundwater recharge, and overall water availability in an ecosystem. Several factors affect the rate of infiltration, including: 1. **Soil Type**: Different soil textures (sand, silt, clay) have varying capacities for infiltration.