 Finite water-content vadose zone flow method

The Finite Water-Content Vadose Zone Flow Method is a modeling approach used to analyze and simulate the movement of water in unsaturated soils, commonly known as the vadose zone. In the vadose zone, water exists in a state between saturation (when the soil is fully saturated with water) and dryness (when the soil has no water). This region is critical for various hydrological processes, such as infiltration, groundwater recharge, and soil moisture dynamics.