Reference soil Romania 10: Cambisol

RO010

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 RO010: Cambisols

VEGETATION: Agrostis tenuis, Phleum montanum, Primula officinalis. ADDITIONAL NOTES ON PROFILE DESCRIPTION: AB - Also slightly gravelly. B - Also slightly gravelly. R - Fractured limestone with soil material penetrations by very thin cracks.

 

Classification

WRB 2014 
Cambisol 
FAO-UNESCO-ISRIC 1974 
Eutric Cambisol  
  
 

 

Local classification:Brown Forest Soil