Saturated Flow

Saturated flow refers to the movement of water through soil or other porous materials when all the available pores are fully filled with water. In this state, the soil cannot absorb any more water, and the flow moves smoothly from areas of higher to lower water pressure or levels. This condition often occurs after heavy rainfall or irrigation when the soil reaches its maximum holding capacity. Understanding saturated flow is important for managing drainage, irrigation, and groundwater resources, as it influences how quickly water moves through the environment and how it interacts with the soil and underground water systems.