Zróżnicowanie składu granulometrycznego jako skutek erozji eolicznej gleb lekkich

Wind erosion is an important soil structure forming factor. Concerning mostly light soils covering for the most part of the European Plains, including Central Poland. Wind erosion susceptibility depends mostly on the aggregate and granulometric structure of the soil. The aim of the paper is to use geostatistical methods to map the changeability of the granulometric structure of the soil on the experimental fi eld in the case of its great variability, and description of the soil cultivation methods which minimizes loss of soil caused by wind erosion.