Reference soil Cuba 14: Calcisol

CU014

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 CU014: Calcisols

Short field description Moderately deep, well drained, brown clay. Small surface cracks, (sub)angular blocky structure, with weathered calcareous fragments. Geology: mid-lower Miocene, formation 'Vazquez': marls, limestones, clays. Geomorphology: marine plain and terrace, abrasive, erosive and undulating.

 

Classification

WRB 2006WRB 1998
Haplic- Calcisol (Endoskeletic)Haplic- Calcisol
20-66 cmcambic horizon
66-90 cmcalcic horizon
-secondary carbonates
0-20 cmochric horizon
20-66 cmcambic horizon
66-90 cmcalcic horizon
-secondary carbonates
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic CalcisolCalcic Cambisol
0-20 cmochric A horizon
20-66 cmcambic B horizon
66-90 cmcalcic horizon
- cmcambic B horizon
- cmochric A horizon
-soft powdery lime
0-20 cmochric A horizon
20-66 cmcambic B horizon
66-90 cmcalcic horizon
-soft powdery lime

 

Local classification:Pardo con carbonato