Saturated hydraulic conductivity

Saturated hydraulic conductivity is a measure of how easily water can flow through soil when the soil is fully saturated with water. Think of it as the soil's ability to let water pass through it when there are no air pockets blocking the flow. Soils with high saturated hydraulic conductivity, like sandy soils, allow water to move quickly, while clay soils with low conductivity slow water down. This property is important for understanding drainage, irrigation, and groundwater movement, helping us predict how water behaves in different soils and environments.