Reference soil Nigeria 19: Phaeozem

NG019

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 NG019: Phaeozems

BRIEF CHARACTERIZATION OF THE SOIL: Very deep well drained red sandy clay, derived from sandstone, with mottling in the subsoil. Tubular pores. Few woody and many fibrous roots at the surface.

 

Classification

WRB 2006WRB 1998
Luvic-Ferralic- Phaeozem (Clayic Chromic)Chromi-Luvic- Phaeozem
25-165 cmargic horizon
-ferralic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Ferrali-Luvic PhaeozemLuvic Phaeozem
0-25 cmmollic A horizon
25-165 cmargic B horizon
-ferralic
0-25 cmmollic A horizon
25-165 cmargillic B horizon
-ferralic

 

Local classification:Alagba Series