Reference soil Cuba 17: Calcisol

CU017

Calcisols occur in regions with distinct dry seasons, as well as in dry areas where carbonate-rich groundwater comes near the surface.

Characteristics

Soils having a (petro-)calcic horizon (horizon with accumulation of secondary calcium carbonates). In addition, they have no diagnostic horizons other than an ochric or cambic horizon, a calcareous argic horizon, or a gypsic horizon beneath a petrocalcic horizon.

Distribution of Calcisols (rough estimation supplied by soilgrids)

 

Reference soil CU017: Calcisols

Short field description: Moderately deep, well drained, dark brown clay. Small surface cracks, (sub)angular blocky structure, very porous, frequent hard calcareous nodules. Geology: midle-high Eocene. Unit A: sandstones, marls, limestones and conglomerate. Geomorphology: pre-mountainous, slightly dissected.

 

Classification

WRB 2006WRB 1998
Haplic- Calcisol (Ruptic Siltic Clayic)Haplic- Calcisol
20-50 cmcambic horizon
50-180 cmcalcic horizon
-secondary carbonates
-lithological discontinuity
0-20 cmochric horizon
20-50 cmcambic horizon
50-180 cmcalcic horizon
-secondary carbonates
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic CalcisolCalcic Cambisol
0-20 cmochric A horizon
20-50 cmcambic B horizon
50-180 cmcalcic horizon
0-20 cmochric A horizon
20-50 cmcambic B horizon
50-180 cmcalcic horizon

 

Local classification:Pardo con carbonato tipico