Reference soil Mozambique 03: Nitisol

MZ003

Nitisols occur mainly in the tropics and subtropics, as well as in areas with a Mediterranean type of climate. They are associated with basic rocks (e.g. basalts) or hard limestone or dolomite deposits.

Characteristics

Soils having a nitic horizon (a horizon with pronounced nut-shaped soil structure and significant amount of active iron) within 100 cm from the soil surface, and gradual to diffuse horizon boundaries between the surface and the underlying horizons. They do not have a ferric, plinthic or vertic horizon within 100 cm from the soil surface.

Distribution of Nitisols (rough estimation supplied by soilgrids)

 

Reference soil MZ003: Nitisols

Brief description of the profile: A very deep, well drained, dark red clay soil, moderately structured.About 2 cm of dry litter at the surface. Original vegetation: Brachystegia woodland ("miombo") -Windspeed measured at 2 meter -Magnetite is present in whole profile -Soft nodules have same colour as soil matrix, inner side of nodules is massive. -Horizon boundaries in subsoil are very diffuse

 

Classification

WRB 2006WRB 1998
Acric-Ferralic- Nitisol (Dystric Rhodic)Ferrali-Rhodic- Nitisol (Dystric)
15-185 cmargic horizon
25-70 cmnitic horizon
-ferralic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Dystri-Rhodic NitisolFerric Acrisol
0-25 cmochric A horizon
15-185 cmargic B horizon
-nitic
0-25 cmochric A horizon
15-185 cmargillic B horizon
-ferric

 

Local classification:Chicunja