Reference soil Kenya 20: Planosol

KE020

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 KE020: Planosols

Classification: aeric or abruptic tropaqualf / Soil fauna: ants and termites. Additional notes on profile description: A1: mottles are grey; also very few fine pores; many white points; E1: mottles: yellowish brown, iron; many white points; also few fine pores; E2: mottles: yellowish brown, iron; massive porous prisms with weak tendency to very coarse longitudinal prisms; many white points; B21ir: iron mottles on peds; many white points; B22t: red rootrust mottles and red and yellow pedrust mottles; B23t: reddish brown rootrust mottles; common medium distinct yellowish coatings on peds; B24: reddish brown rootrust mottles; common medium distinct yellowish and common fine faint dark grey coatings on peds; locally silty and ash-like material.

 

Classification

WRB 2006WRB 1998
Umbric-Alic- Planosol (Albic Clayic)Umbri-Alic- Planosol (Albic)
0-46 cmumbric horizon
46-66 cmalbic horizon
74-105 cmargic horizon
-abrupt textural change
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Albi-Umbric PlanosolHumic Planosol
0-46 cmumbric A horizon
46-66 cmalbic E horizon
74-105 cmargic B horizon
-abrupt textural change
-stagnic
0-46 cmumbric A horizon
46-66 cmalbic E horizon
74-105 cmargillic B horizon
-abrupt textural change
-hydromorphic