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Par Collection Par Auteur- MIDRIAK, R. (3)
- Geography of Europe (3)
- Conservation des sols ; Dégradation des sols ; Géographie de l'Europe ; Géographie des sols ; Protection de la nature ; Pédogenèse ; Pédosphère ; Sol ; Sol cultivé ; Sol forestier ; Tchécoslovaquie (1)
- Erosion des sols ; Erosion par l'eau ; Etagement ; Forêt ; Géographie de l'Europe ; Karpaty ; Montagne ; Tchécoslovaquie (1)
- Erosion des sols ; Erosion pluviale ; Géographie de l'Europe ; Géomorphodynamique ; Ruissellement ; Régionalisation ; Sol ; Sol forestier ; Tchécoslovaquie ; Unité géomorphologique (1)
- Potencialna erozia pôdy vo vysokych pohoriach ceskoslovenskych Karpat. (Potential soil erosion in high moutains of Czechoslovak Carpathians) (1)
- Pôda-jeden zo zakladnych faktorov zivotného prostredia, jej devastacia a ochrana. (Soil one of basic environmental factors, its devastation and protection) (1)
- Regionalizacia geomorfologickych celkov CSSR z hladiska potencialnej erozie lesnej pôdy. (Regional categorization of Czechoslovak geomorphologic units on the basis of a potential erosion of forest soils) (1)
- Regionalizacia geomorfologickych celkov CSSR z hladiska potencialnej erozie lesnej pôdy. (Regional categorization of Czechoslovak geomorphologic units on the basis of a potential erosion of forest soils)
- Important data on potential erosion of forest soils by running water are summarized in all 177 geomorphological units in Czechoslovakia. The Frevert-Zdrazil method of erosion calculation modified by O. Stehlik is applied. The erosion intensity may
- Position of pedosphere in geography, functions of soil in environment, soil destruction and devastation in Caechoslovakia. Problems of agricultural and forest soil conservation. (MS).
- Intensity of potential soil losses due to erosion by running water is very high in the Western Carpathians. The average potential loss of soil mantel is 7,29mm per annum. In the upper part of forest zone from 1000m a.s.l. to the contemporaneous