Reference soil Malaysia 58: Cambisol

MY058

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 MY058: Cambisols

A red yellow podzolic soil of poorly crystallized kaolinit ineralogy with admixture of poorly crystallized vermiculite, derived from non-homogeneous hard cretaceous shale. The soil had once been used for shifting cultivation (hill rice). There are mottles in EBw and Bw (gray and weak red, the latter probably weathered parent material). The 2Bs contains platy material, probably iron oxides, derived from fossil accumulation in shale. Apart from gray mottles, the 3Bws has got some small quartz pebbles (dark gray-white). The Stass series is suitable for agriculture, but needs to be adequately fertilized for most crops. (additional climatic data: days with precipitation >0,1 mm)

 

Classification

WRB 2014 
Cambisol 
FAO-UNESCO-ISRIC 1974 
Dystric Cambisol  
  
 

 

Local classification:Stass series