Reference soil Kenya 25: Planosol

KE025

Planosols occur in level landscapes throughout the world often associated with broad river valleys.

Characteristics

Soils having an eluvial horizon, the lower boundary of which is marked. within 100 cm from the soil surface, by an abrupt textural change associated with stagnic properties above that boundary. The feature of albeluvic tonguing, however, is lacking.

Distribution of Planosols (rough estimation supplied by soilgrids)

 

Reference soil KE025: Planosols

A very shallow to shallow soil (20-30 cm of depth) with many dead rootlets in B21 horizon; strong surface sealing.

 

Classification

WRB 2006WRB 1998
Solodic- Planosol (Albic Calcaric Clayic)Calcari-Albic- Planosol
15-26 cmalbic horizon
26-90 cmargic horizon
-calcaric
-abrupt textural change
-stagnic colour pattern
-reducing conditions
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Albi-Eutric PlanosolEutric Planosol
0-15 cmochric A horizon
15-26 cmalbic E horizon
26-90 cmargic B horizon
-abrupt textural change
-stagnic
0-15 cmochric A horizon
15-26 cmalbic E horizon
26-90 cmargillic B horizon
-hydromorphic