Values of a quantitative index of erosion resistance (namely, the stre
am erosion velocity) are determined for the genetic horizons of the pr
incipal soil groups of Tajikistan. A relationship is demonstrated betw
een stream erosion velocity and stability of soil aggregates in water,
the cohesiveness of the soils, and their content of roots. It is show
n that a familiar equation for stream erosion velocity, developed prev
iously for plains soils, can be used to evaluate quantitatively the er
osion resistance of the mountain and piedmont soils of Tajikistan.