بيدولوجية بعض ترب منخفضات الصحراء الغربية من العراق

Characterization and classification of some depression soil in the western desert were studied. The following conclusion: 1- Calcification processes are the important one, while topography is the active factor in the desert zone. 2- According to Morphology, Argillic horizons were investigated in some depressions. This horizon fromed under pluvial periods. 3- All the soils were good fetrtile, with good water and soil management, and it classified under class three.