Reference soil Kenya 14: Phaeozem

KE014

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 KE014: Phaeozems

A strongly calcareous, moderately well drained soil derived from fine-grained sandstones, with common moderate clay cutans below 30 cm and a weak surface sealing (5 mm); inactive termite mounds (5-10 m diameter, 1-2 m height) appear. (R3 pg 215)

 

Classification

WRB 2006WRB 1998
Luvic- Phaeozem (Calcaric)Calcari-Luvic- Phaeozem
0-30 cmmollic horizon
30-110 cmargic horizon
-calcaric
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Calcari-Luvic PhaeozemLuvic Phaeozem
0-30 cmmollic A horizon
30-110 cmargic B horizon
-calcareous
0-30 cmmollic A horizon
30-110 cmargillic B horizon