Supplementary material to "Agropedogenesis: Humankind as the 6<sup>th</sup> soil-forming factor and attractors of agrogenic soil degradation"

qualifiers and master properties.Other frequent examples of soil class changes are presented in (Dudal, 2004) major erosion, the soil taxonomic group changed due to a strong decrease in the Ah / Ap horizon depth, which led to new depletion of easily erodible materials.It reaches steady state conditions when erosion becomes equal to soil genesis.After Supplementary Fig. 1: Soil depth decrease due to erosion.The erosion rate decreases with cultivation duration due to