Reference soil New Zealand 02: Cambisol

NZ002

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 NZ002: Cambisols

LAND USE: pastoral land for intensive fat stock production (mainly fat lambs); some cash crops; well suited to intensive wheat farming

 

Classification

WRB 1998 
Hyperdystric- Cambisol 
  
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Silti-Dystric CambisolDystric Cambisol

 

Local classification:Strongly leached southern yellow-brown earth; Waikiwi silt loam