Reference soil Cuba 11: Cambisol

CU011

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 CU011: Cambisols

Short field description: Shallow, well drained, dark yellowish brown clay. There are mottles, hard calcareous and soft managanese nodules, and a massive fragipan which is weakly cemented. Geology: Cretaceous superior, Campaniano-maestrichtiano. Formation: San Juan y Martinez, biodetritic limestone, conglomerate, marls, at the site igneous rocks. Geomorphology: marine plains and terrace abrasive and abrasive accumulative, undulating and slightly undulating.

 

Classification

WRB 2006WRB 1998
Haplic- Cambisol (Hyposodic Clayic)Hyposodic- Cambisol
18-44 cmcambic horizon
0-18 cmochric horizon
18-44 cmcambic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Eutric CambisolEutric Cambisol
0-18 cmochric A horizon
18-44 cmcambic B horizon
- cmcambic B horizon
- cmochric A horizon
0-18 cmochric A horizon
18-44 cmcambic B horizon

 

Local classification:Pardo sin carbonato