Reference soil Peru 24: Chernozem

PE024

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 PE024: Chernozems

Short field description Soil profile located in a lacustrine plain with meandering rivers. It is a deep, depending on a variable water table, moderate drained, very dark greyish brown to black, loam to silty clay loam. The pasture land has a dense grass cover and is used for sheep grazing.

 

Classification

WRB 2006WRB 1998
Calcic-Endofluvic-Vermic- Chernozem (Sodic Pachic Siltic)Silti-calcic horizon- Chernozem (Vermic)
0-123 cmmollic horizon
28-48 cmcalcic horizon
-calcaric
-fluvic
-lithological discontinuity
0-123 cmmollic horizon
28-48 cmcalcic horizon
-calcaric
-fluvic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Sodi-Calcic ChernozemCalcic Chernozem sodic
0-123 cmmollic A horizon
28-48 cmcalcic horizon
- cmmollic A horizon
-fluvic
-sodic
0-123 cmmollic A horizon
28-48 cmcalcic horizon
-soft powdery lime

 

Local classification:Suelo Petreria