This paper has studied as soil unit the stagnic, calcaric faeoziom from Grecesti, Dolj that belongs to the Jiu River hydrografic Basin. There was established that this soil occupies in the central zone a small surface yet it is identified in large areas in the superior part of the southern versants due to the better drainage the eluviations processes have been reduced and this is the reason why a B horizon does not appear. The physic-chemical processes that characterizes the soil enframe this soil into the middle productive soils; in order to enhance its productive potential we have to make deep tillages, good fertilization. By its specific, this paper can be used by the loco farmers in order to enhance their yields.

faeoziom; soil profile; texture; structure; fertility

Presentation: oral