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The aim of this paper is to study the physical properties of soils as key factors in favoring pluvial denudation and the spatial distribution of degraded areas through hydric erosion. The soil types from the degraded areas and the soils physical properties that influence the erodibility were analised in the south-western part of the Seca?e Plateau (Romania). Field geomorphologic and pedological observations and laboratory physical analyzes of soil samples (texture, permeability, porosity and degree of compaction) ...