Reference soil United States of America 21: Phaeozem

US021

Phaeozems occur all over the world, but especially on the more moist side of the steppe regions, bordering Chernozems.

Characteristics

Soils having a mollic horizon (deep, brownish or blackish surface horizon with a significant accumulation of organic matter and high base saturation); a base saturation of 50 percent or more between 25 and 100 cm from the soil surface; a calcium carbonate-free soil matrix at least to a depth of 100 cm from the soil surface, or to a contrasting layer between 25 and 100 cm; no diagnostic horizons other than an albic, argic, cambic or vertic horizon, or a petrocalcic horizon in the substratum.

Distribution of Phaeozems (rough estimation supplied by soilgrids)

Reference soil US021: Phaeozems

Classification

WRB 1998 
Luvi-Gleyic- Phaeozem (Siltic) 
  
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Luvi-Gleyic PhaeozemGleyic Phaeozem

 

Local classification:Haig silty clay loam