Reference soil Russian Federation 06: Chernozem

RU006

Chernozems are typically found in the long-grass steppe regions of the world, particularly in Eastern Europe and North America (Canada and the USA).

Characteristics

Soils having a very dark mollic horizon (thick, brownish or blackish surface horizon with a significant accumulation of organic matter and high base saturation) and secondary carbonates within 50 cm of the lower limit of the Ah horizon, but within 200 cm from the soil surface. They have no petrocalcic horizon between 25 and 100 cm from the soil surface, no secondary gypsum and no uncoated sand and silt grains on structural pedfaces

Distribution of Chernozems (rough estimation supplied by soilgrids)

 

Reference soil RU006: Chernozems

Location: approx. 110km E of Kursk A very dark grey to black topsoil, rich in organic matter, overlying a light yellowish brown calcareous subsoil. Structure is prismatic to subangular blocky in the lower part and dominantly crumb in the upper part due to high faunal activity (earth worms). Below 100 cm accumulation of calcium carbonate occurs in concretionary and pseaudomycelia form. In the Ah3 and ABk horizons, two colours are dominant. In the Ah3 and ABk horizons this is due to mottling (mottle colour 10YR 4/2). In the ABk horizon material of Ah3 (10YR 5/2.5) is tonguing into material of Bwk (10YR 6/4). Climate: x = depth (cm) of <0 degrees C penetration; snow cover height 42 cm; length of frost-free days 164

 

Classification

WRB 2014 
Chernozem 
FAO-UNESCO-ISRIC 1974 
Calcic Chernozem  
  
 

 

Local classification:Typical Chernozem