Reference soil Cuba 08: Cambisol

CU008

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 CU008: Cambisols

Short field description: Moderately deep, well drained, light brown clay. Flagstone of flattened hard rock are present in the soil from 120 cm and deeper. Variety: Cu 323 68, plant ratoon-yield 150 ton/ha, first and second ratoon 120 ton/ha, third and fourth ratoon-100 ton/ha. Geology: Neogene Era, mid-higher undifferentiated Eocene. Bijabo formation: conglomerate, sandstone, limestone. Geomorphology: undulating erosive denudative plains.

 

Classification

WRB 2006WRB 1998
Haplic- Cambisol (Calcaric Clayic)Calcaric- Cambisol
22-80 cmcambic horizon
0-22 cmochric horizon
22-80 cmcambic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Calcaric CambisolCalcic Cambisol
0-22 cmochric A horizon
22-80 cmcambic B horizon
-calcareous
0-22 cmochric A horizon
22-80 cmcambic B horizon

 

Local classification:Fersialitico pardo rojizo