In the article, the object of study of the Ganja-Gazakh steppe is widely distributed in the following areas: Mountain-forest brown soils washed from carbonates (Haplic Castanozems). Mountain-brown soils (Kastonozems) from the forest, washed from carbonates. Under the forest, carbonate mountain-brown soils (Kastonozems). Wild mountain-forest brown soils (Mollic Leptosols Eutric). Carbonate mountain-black soils (Chernozems, 1350 m). Dark mountain gray-brown soils (Castanozems). Ordinary mountain gray-brown soils (Castanozems). Light mountain gray-brown soils (Castanozems). Dark gray-brown soils (Haplic Castanozems Chromic). Common gray-brown soils (Haplic Castanozems Chromic). Dark gray-brown, Light gray-brown soils (Castanozems). Wetland-meadow soils (Gleysols). Field-soil-erosion researches were carried out, numerous sections were made in these soils and samples were taken from different genetic layers and laboratory analyzes were carried out, their granulometric composition, agro-chemical and water-physical properties were studied and studied. solid phase density, hygroscopic moisture, soil swelling ability, its compaction capacity, pH.In water suspension, the sum of absorbed bases, m.eq., the sum of absorbed bases, Na%, Carbonate content, total nitrogen and humus content were determined and their erosion limits were determined.