Reference soil Samoa 05: Cambisol

WS005

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 WS005: Cambisol

A fine latosolic soil at south end of banana fertilizer trial, consisting of "collo-alluvium" derived from clcareous tuff. In the B2 horizon saprolite is present (colour dry 5 YR 3/3). (The precipitation data of Lotofaga are only APPROXIMATE values; additional climatic data: Temperature (C) Faleolo Airport: Time Mean Max Min years Jan 26.7 30.3 24.0 1975-77 Jul 25.9 29.9 23.9 1974-76)

 

Classification

WRB 2014 
Cambisol 
 

 

Local classification:Vini clay