OBSERVATIONS ON THE PRESENCE RHODI-EUTRIC CAMBISOLS (TERRA ROSSA) IN ROMANIA

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]

PARICHI M., STĂNILĂ A. L., MUŞAT M. 2013, OBSERVATIONS ON THE PRESENCE RHODI-EUTRIC CAMBISOLS (TERRA ROSSA) IN ROMANIA. Scientific Papers. Series A. Agonomy., Vol. LVI, ISSN 2285-5785, 79-82.


The publisher is not responsible for the opinions published in the Volume. They represent the authors’ point of view.
© 2012 Scientific Papers. Series A. Agronomy. All Rights Reserved. To be cited: Scientific Papers. Series A. Agronomy
Powered by INTEL TECH DEVELOPMENT.