What condition describes soil that is fully soaked with water?

Soil saturation refers to the condition in which all the pores within the soil are completely filled with water. In this state, the soil can no longer hold any additional water and becomes waterlogged. This is an important concept in agriculture and environmental management since saturated conditions can affect plant growth, microbial activity, and the overall health of the soil ecosystem.

Understanding soil saturation is crucial for fertilizer applicators, as applying fertilizers in saturated conditions can lead to runoff and nutrient loss, impacting both crop yield and environmental quality. It is essential for practitioners to recognize when soils are saturated to avoid applying fertilizers under unsuitable soil conditions.