Published in Scientific Papers. Series A. Agonomy., Vol. LVI
Written by Mihai PARICHI, Anca-Luiza STĂNILĂ, Marian MUŞAT
Rhodi-eutric cambisols is a dominating in the mediterranean regions, its presence being connected to limestone that is the most times jurassic. The soil origin material is represented by the residues of the limestone dissolving. Rhodi-eutric cambisols also appears locally in the west side of the country and in submediterranean climate conditions (Banatului Mountains) and in climate conditions (humid climate) with oceanic influences (Apuseni Mountains) and in the most frequent cases associated with rendzic leptosols, eutri-lithic leptosols and rocks. From the most recent field and laboratory data results that the rhodi-eutric cambisols soils develop also in present if some morfohidroclimatic conditions are fulfilled.
[Read full article] [Citation]
limestone
