Reference soil Nigeria 04: Lixisol

NG004

Lixisols occur dominantly in the drier parts of the tropics and subtropics. Their high base status is partly due to less leaching, partly to admixture from airborne dust from adjacent desert regions.

Characteristics

Soils having an argic horizon (a subsurface horizon with a distinct higher clay content than the overlying horizon), which has a cation exchange capacity of less than 24 cmolc per kg in some part, either starting within either: 100 cm from the soil surface, or 200 cm from the soil surface if the argic horizon is overlain by loamy sand or coarser textures throughout. They have a base saturation (total amount of Ca, Mg, K and Na with respect to the cation exchange capacity) of 50 percent or more in the major part between 25 and 100 cm from the soil surface.

Distribution of Lixisols (rough estimation supplied by soilgrids)

 

Reference soil NG004: Lixisols

Physiographic unit: Mid section of slope between small plateau and valley bottom in rolling country. Drainage: Well to excessively drained. Parent rock: Banded para-gneiss, multicoloured with grey, dark greenish grey, yellowish and reddish bands of a few mm, dip approximately 45% E, strongly weathered. CPCS classification: Sol ferrugineux tropical lessive General aspect: Very shallow brownish sandy soil over parent para-gneiss. Source of climate data: Agroclimatological data Africa 1, FAO. Rome 1984.

 

Classification

WRB 2006WRB 1998
Leptic-Cutanic- Lixisol (Chromic)Chromi-Leptic- Lixisol
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic Lixisol rudicFerric Luvisol stony
- cmargic B horizon
- cmochric A horizon
- cmargillic B horizon
- cmochric A horizon

 

Local classification:Balogun Series