Reference soil Malaysia 59: Cambisol

MY059

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 MY059: Cambisols

A moderately deep, imperfectly drained profile with clayey texture and mixed mineralogy (kaolinite with a mixture of chlorite/vermiculite). This red-yellow podzolic soil, derived from laminated shales of Cretaceous age, is situated near hill summit of rolling to hilly late Pleistocene peneplain. The surface is covered by an O-layer (3cm), consisting of decomposed litter, with abrupt boundary to next horizon. Below 64 cm iron cemented laminated pieces of shale appear increasing with depth. The Cg (coloured 5 YR 6/8 and 10 YR 7/2) consits mainly of shale varying in degree of weathering. Colour mottling below 64 cm indicating hydromorphic conditions may partly be caused by persistence of gray colours of the parent material. Only a few clay cutans are observed in thin section. The profile may have been truncated because an E horizon is not present. The present A horizon may thus be part of the former B, although this is difficult to prove at present. The soil is suitable for a wide variety of crops, but the drainage must be improved for sensitive rops such as pepper. (additional climatic data: days with precipitation > 0,1mm)

 

Classification

WRB 2014 
Cambisol 
FAO-UNESCO-ISRIC 1974 
Gleyic Cambisol  
  
- cmcambic B horizon
-hydromorphic
-mottles with chroma <2
 

 

Local classification:Semongok series