Reference soil Nigeria 09: Alisol

NG009

Alisols occur in the tropics and subtropics, and in the warm temperate regions of the world in relatively young landscapes. The high level of exchangeable aluminium in these soils is caused by rapid weathering of secondary high-activity clays such as vermiculite and smectite.

Characteristics

Soils having an argic horizon (a subsurface horizon with distinct higher clay content than the overlying horizon), which has a cation exchange capacity of 24 cmolc per kg clay or more, and which starts either within 100 cm from the soil surface, or within 200 cm from the soil surface if the argic horizon is overlain by loamy sand or coarser textures throughout. They have "alic" properties (high content of exchangeable aluminium) in the major part between 25 and 100 cm from the soil surface; moreover, only such diagnostic horizons as an ochric, albic, andic, ferric, nitic, plinthic, or vertic horizon are present.

Distribution of Alisols (rough estimation supplied by soilgrids)

 

Reference soil NG009: Alisols

Brief description on the profile: A deep reddish clayey soil with a thin blackish sandy surface horizon. Structure weak, fine subangular blocky down to 26 cm, strong fine subangular blocky below.From 50-145 cm clay cutans. Many (sub)rounded hard Fe/Mn nodules down to 145 cm, generally less than 1 cm across. Clay minerals are predominantly kaolinite. Location: Roadside cut, E of Ago-Are-Kishi road, 300 m S of MP 29 from Kishi. Physiographic unit: Part of a low ridge close to a subsidiary crest grading towards a U shaped valley. No recent shifting cultivation. Base saturation is >35% within critical depth. INRA classification: Sol ferrugineux tropical lessive a concretions Additional notes on the profile description: B1cn: Some ferruginized schist fragments. 2B2tcn(original designation): Prominent stress cutans around gravels and saprolithic in patches with yellowish streaks; few ferruginized schist fragments. 2B3: Yellowish and brownish mottles and streaks; soft saprolite without rock structure; pseudomorphs of feldspar. Climate data source: Agroclimatological data Africa 1, FAO. Rome 1987

 

Classification

WRB 2006WRB 1998
Pisoplinthic-Cutanic- Alisol (Profondic Chromic)Chromi-Profondic- Luvisol (Dystric)
26-145 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic Alisol skeleticOrthic Acrisol petric
0-26 cmochric A horizon
26-145 cmargic B horizon
0-26 cmochric A horizon
26-145 cmargillic B horizon
-ferric

 

Local classification:Sepeteri Series