Author(s): Mihai Parichi | Anca-Luiza Stănilă | Gheorghe Herişanu
Journal: Present Environment and Sustainable Development
ISSN 1843-5971
Volume: 5;
Issue: 1;
Start page: 113;
Date: 2011;
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Keywords: Barlad basin | erosion | texture
ABSTRACT
Through its relief variety coefficient, the Barlad Plateau is registered 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 Plateau. Their physical,hydro-physical and chemical characteristics, as the relief conditions, to which the brainless usage mode is added, have increased considerably the vulnerability to erosion. In the present, on big surfaces of land, the erosion has even carried off the B horizon of the soils, coming to work even in the C horizon
Journal: Present Environment and Sustainable Development
ISSN 1843-5971
Volume: 5;
Issue: 1;
Start page: 113;
Date: 2011;
VIEW PDF
DOWNLOAD PDF Original pageKeywords: Barlad basin | erosion | texture
ABSTRACT
Through its relief variety coefficient, the Barlad Plateau is registered 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 Plateau. Their physical,hydro-physical and chemical characteristics, as the relief conditions, to which the brainless usage mode is added, have increased considerably the vulnerability to erosion. In the present, on big surfaces of land, the erosion has even carried off the B horizon of the soils, coming to work even in the C horizon
