Reference soil Brazil 08: Nitisol

BR008

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 BR008: Nitisols

Brief field description: Very deep, well drained, dark reddish brown clay soil derived from basic rock; slightly cracking when dry. Soil formed in weathered products of basalt of the 'Serra Geral' formation, Jurassic/Cretaceous. The sorptivity for water is high throughout the profile (although relatively less high in the first 65 cm). *) Brazilian classification: Latossolo Roxo Humico Distrofico. Reference soil BR 08 is comparable to soil profile 10 III RCC.

 

Classification

WRB 2006WRB 1998
Ferralic-Vetic- Nitisol (Humic Alumic Rhodic)Veti-Humic- Nitisol (Alumic Rhodic)
22-265 cmnitic horizon
0-44 cmochric horizon
22-265 cmnitic horizon
-strongly humic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Rhodic FerralsolHumic Ferralsol
0-44 cmumbric A horizon
22-265 cmferralic B horizon
- cmferralic B horizon
- cmumbric A horizon
-strongly humic
0-44 cmochric A horizon
22-265 cmoxic B horizon
-high organic matter content in the B horizon

 

Local classification:Latossolo Roxo Húmico distrófico