Soil permeability

Soil permeability refers to how easily water can pass through the soil. It depends on the soil's size, texture, and structure—coarse soils like sandy or gravelly types allow water to flow quickly, while fine soils like clay restrict movement. Permeability affects things like drainage, plant growth, and the stability of underground structures. High permeability means water moves easily, reducing waterlogging but potentially reducing groundwater recharge. Low permeability means water moves slowly, which can lead to pooling or flooding. Understanding soil permeability is essential for managing agriculture, construction, and environmental concerns effectively.