ASPECTS CONCERNING SOIL EROSION IN THE BARLAD RIVER BASIN

Through its relief variety coefficient, the Barladului Highlands is booked as a standard territory, pointing a hilly region of which soil cover presents a pronounced diversity. Considering all this, it has two main corresponding pedogenetic areas: cernisoils and luvisoils. The first characterize mostly Colinele Tutovei, while the luvosoils appear dominantly in the Central Moldavian Highlands. Their physical, hydro-physical and chemical characteristics, as the relief conditions, to which is added the brainless usage mode have increased considerably the vulnerability to erosion. At present on big surfaces of land, erosion has even carried off the B horizon of the soils, coming to work even in C horizon.