Answer:
Step-by-step explanation:
It is called runoff or runoff to the stream of water that is poured when exceeding its deposit or natural or artificial channel. In hydrology, runoff refers to the sheet of water that circulates on the surface in a drainage basin, that is, the height in millimeters of the drained and extended rainwater. Normally, precipitation is considered less real evapotranspiration and infiltration of the soil system. According to Horton's theory, it is formed when rainfall exceeds the infiltration capacity of the soil. This is only applicable in soils of arid zones and torrential rainfall. This deficiency is corrected with the theory of saturation, applicable to soils in areas of high and constant rainfall. According to this theory, runoff will be formed when the compartments of the soil are saturated with water.