Reference soil Ghana 02: Planosol

GH002

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 GH002: Planosols

Planosol

 

Classification

WRB 2006WRB 1998
Luvic-Endofluvic- Planosol (Sodic Arenic)Endosodi-Endogleyic- Plinthosol (Luvic Arenic)
67-145 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Endosodi-Eutric PlanosolSolodic Planosol sodic
0-24 cmochric A horizon
67-145 cmargic B horizon
-abrupt textural change
-sodic
0-24 cmochric A horizon
67-145 cmcambic B horizon
-abrupt textural change
-hydromorphic

 

Local classification:Regosolic Groundwater Laterite, Doyum Series