Reference soil Namibia 04: Phaeozem

NA004

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 NA004: Phaeozems

Phaeozem HUMAN INFLUENCE: topsoil is disturbed and grass vegetation is seriously impeded by overgrazing

 

Classification

WRB 2006WRB 1998
Haplic- Phaeozem (Pachic)Pachic- Phaeozem
0-50 cmmollic horizon
50-90 cmcambic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Pachi-Haplic PhaeozemHaplic Phaeozem
0-50 cmmollic A horizon
50-90 cmcambic B horizon
0-50 cmmollic A horizon
50-90 cmcambic B horizon

 

Local classification:Dunkelbrauner Talboden der Dornbuschsavanne auf kalklosem Substrat (Scholz, 1962)