S is the soil texture determines the soil media that is important in controlling the amount of water that penetrates into the ground. Deposits of clay loam, gravel, loam, non-shrinking and nonaggregated clay, sand, sandy loam, and silty loam constitute the soil map. Gravel, sand, and sandy loam showed the maximum rate (Aller et al., 1987). Sand was found in the northern and southern regions of the study area, as indicated by the soil media layer. Sand also showed high permeability.