Аннотации:
Quantity of mechanical and chemical denudation, estimated on the load of suspended sediments and dissolved subtance are examined. The role of zonal and non-zonal factors (relief, rocks, human activity) in spatial changes of these types of denudation is fixed. Spatial variability of denudation has a complicated structure and in different natural-anthropogenic conditions repeatedly reacts on chages of controlling it factors. Maximums, connected with highly mastered regions of temperate belt and subtropics-tropics regions are revealed. © 2005 A.P. Dedkov, V.I. Moszherin, A.N. Sharifullin, P.P. Denmukhametov.