Reference soil Italy 17: Calcisol

IT017

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 IT017: Calcisols

The profile shows a greyish yellow soil of clay loam texture with a well-developed calcic horizon below the A-horizon. In this subsurface horizon cutans, probably calcitans, occur. With depth vertic properties (intersecting slickensides) increase. At least part of the vertic properties are of gegenetic origin. banded sandy inclusions reflect the original stratification of the parent material. Parent material: shales with inclusions of Miocene age ('argillic caotiche'). Human influence: quarrying. References: Spaargaren, O., 1979, 'Weathering and Soil Formation in a Limestone Area near Pastena (Fr., Italy)', University of Amsterdam, no.30 (Fys. Geogr. en Bod. Lab.). Profile is similar to profile Sp/166 of Spaargaren (1979).

 

Classification

WRB 2014 
Calcisol 
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Verti-Haplic Calcisol phreaticCalcic Cambisol phreatic
- cmcalcic horizon
- cmcambic B horizon
- cmochric A horizon
-vertic
- cmcalcic horizon
- cmcambic B horizon
- cmochric A horizon

 

Local classification:Suolo bruno calcareo