Reference soil Nigeria 21: Phaeozem

NG021

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 NG021: Phaeozems

BRIEF CHARACTERIZATION OF THE SOIL: Moderately deep, well drained brown sandy clay, derived from gneiss, with hard spherical magniferous concretions in the subsoil.

 

Classification

WRB 2006WRB 1998
Luvic-Ferralic- Phaeozem (Clayic Chromic)Chromi-Luvic- Phaeozem
25-175 cmargic horizon
-ferralic
-ferralic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Ferrali-Luvic PhaeozemLuvic Phaeozem
0-25 cmmollic A horizon
25-175 cmargic B horizon
0-25 cmmollic A horizon
25-175 cmargillic B horizon
-ferralic

 

Local classification:Iwo Series