Reference soil Kenya 49: Phaeozem

KE049

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 KE049: Phaeozems

Small fields of 3 x 3m dissected by ditches for drainage, rainfed irrigation. Slides: 10,082 - 10,088.

 

Classification

WRB 2006WRB 1998
Gleyic- Phaeozem (Pachic Clayic Novic)Pachi-Endogleyic- Phaeozem
140-165 cmcambic horizon
25-140 cmmollic horizon
-fluvic
-gleyic colour pattern
-reducing conditions
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Fluvi-Gleyic Phaeozem inundicGleyic Phaeozem
0-25 cmochric A horizon
25-55 cmmollic A horizon
55-165 cmcambic B horizon
-fluvic
-gleyic
0-25 cmochric A horizon
25-55 cmmollic A horizon
55-165 cmcambic B horizon
-hydromorphic