Water Flow in Soils

Water flow in soils is the movement of water through the spaces between soil particles. When it rains, some water is absorbed by the soil, while excess water moves downward due to gravity. This process can be influenced by soil type; for example, sandy soils drain quickly, while clay soils hold water longer. Water can also flow sideways, especially in saturated conditions, affecting nearby plants and groundwater levels. Understanding this movement is essential for agriculture, landscaping, and managing water resources effectively.