Reference soil Jamaica 02: Nitisol

JM002

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 JM002: Nitisols

Evapo-transpiration data are from Smithfield. Parent material consist of weathered residue from chalky limestrone. Haplic Luvisol (FAO, 1988) Ultic Hapludalf (Soil Taxonomy, 1990) by soil reaction field kit

 

Classification

WRB 2006WRB 1998
Acric- Nitisol (Eutric Novic)Eutric- Nitisol
38-170 cmargic horizon
38-170 cmnitic horizon
-abrupt textural change
0-17 cmochric horizon
38-170 cmargic horizon
38-170 cmnitic horizon
-abrupt textural change
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Eutri-Haplic NitisolEutric Nitosol
0-17 cmochric A horizon
38-170 cmargic B horizon
-abrupt textural change
-nitic
0-17 cmochric A horizon
37-170 cmargillic B horizon
-abrupt textural change
-weatherable minerals

 

Local classification:Copse clay loam