Soil Water Balance

Soil water balance refers to the balance between the amount of water entering and leaving a soil system. It includes factors like precipitation (rainfall), evaporation (water loss to the air), and plant uptake (water used by plants). When the water entering the soil equals the water leaving, the soil is in balance. If more water enters, it can lead to saturation or flooding; if more leaves, the soil can dry out. Understanding this balance helps in managing agricultural practices, water resources, and environmental conservation effectively, ensuring healthy ecosystems and crop production.