Reference soil Jamaica 06: Cambisol

JM006

Cambisols occur mainly in the temperate and boreal regions of the world, where the soil’s parent material is still young or where low temperatures slow down the processes of soil formation.

Characteristics

Soils having either a cambic horizon (a horizon showing evidence of alteration with respect to the underlying material), or a mollic horizon overlying a subsoil, which has a base saturation of less than 50 percent in some part within 100 cm from the soil surface, or one of the following diagnostic horizons within the specified depth: an andic, vertic, or vitric horizon starting between 25 and 100 cm; a (petro-)plinthic or salic horizon starting between 50 and 100 cm, in absence of loamy sand or coarser textures above these horizons.

Distribution of Cambisols (rough estimation supplied by soilgrids)

 

Reference soil JM006: Cambisols

REFERENCES: Hafkenscheid R. 2000. Hydrology and biogeochemistry of tropical montane rain forests of contrasting stature in the Blue Mountains, Jamaica. Thesis Free University Amsterdam

 

Classification

WRB 2006WRB 1998
Endoleptic- Cambisol (Alumic Humic)Dystri-Endoleptic- Cambisol
20-88 cmcambic horizon
-continuous rock
0-20 cmochric horizon
20-88 cmcambic horizon
-continuous hard rock
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Dystric CambisolDystric Cambisol
0-20 cmochric A horizon
20-88 cmcambic B horizon
-strongly humic
0-20 cmochric A horizon
20-88 cmcambic B horizon