LAND DEGRADATION AND SOIL CONSERVATION ON THE MOLDAVIAN PLATEAU, ROMANIA

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Abstract:

The Moldavian Plateau, located in eastern Romania and extending about 27,000 square kilometers, is one of the most severely eroded agricultural areas in the country. Clayey-sandy Miocene-Pliocene layers with a gentle gradient of 7-8 m km-1 NNW-SSW have outcropped from sedimentary substratum (Jeanrenaud, 1971). The climate is temperate continental with a mean annual temperature of 8.0 - 9.8 0C. Average annual precipitation varies from about 460 millimeters at the lower elevation in the southern part to 670 millimeters in the central and northwestern area with elevations up to 587 meters. Natural vegetation cover was drastically changed by man particularly during the last two centuries. Mollisols and argiluvisols (forest soils) are among the most common soils and have been used for crop production. The main land use stratification is cropland (58%), pastures and meadows (16%) and forest (13%).

Keywords: LAND DEGREDATION AND SOIL CONSERVATION ON THE MOLD

Document Type: Research article

Publication date: 2008-01-01

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