Soil taxa (ex, Great Group of Soil Taxonomy):
Russian classification: soddy podzolic heavy loamy on heavy mantle loam.
FAO: podzoluvisols
Profile description.( soil pit N43, 1922 year)
A0 – 0-2, sod cover.
A1 – 2-14 cm, gray-brown, lower part of a lighter colouring; platy structure; very frequently permeated by plant roots. Transition to the next horizon is gradual.
A2 – 14-22 cm. Whitish; the colour is not quite homogeneous, there are very small iron nodules. High porosity, relatively high number of earth-worm channels. Fine-platy structure, colour of inner parts of aggregates is not homogeneous. Transition to the next horizon is gradual.
B1 – 22-50 cm. Dark-brown with bleached veins, nutty structure, ped faces slightly covered with whitish powdering; weakly bleaching in pores and fissures.
B2 – 50-120 cm. Yellow-brown, more light than previous, prismatic structure, porous. Sides of soil particles and the surfaces of cracks are covered with a brown cutans, not abundant whitish powdering of cracks, abundance of Mn black spots.
B3 – 120-160 cm. Yellowish light-brown, the colour is lighter than that of B2; abu-
dance of rusty spots. Cloody weak structure, very compact; walls of cracks are filled with brown-red cutans. Single till boulders.
B3 – 160-230 cm. Predomination of rusty colour , which is lighter than that of the upper horizon. Cracks are very few; their walls are covered with a darker and thick cutans. The number of boulders is higher than in the upper horizon. Distinct diagonal banding is observed in some parts of the horison, very compact, porous inner part of peds, single plant roots
Thickness of root layer - 120 cm.
Water holding capacity of the arable horizon – 36%
Soil granulometric composition, physical properties and bulk analysis results (incl. total C and N ) in 1922 soil pit are available.