Reference soil Malaysia 54: Fluvisol

MY054

Fluvisols typically are young soils in alluvial, deltaic, lacustrine, or marine deposits, and occur all over the world.

Characteristics

Soils having fluvic soil material starting within 25 cm from the soil surface and continuing to a depth of at least 50 cm from the soil surface. They have no diagnostic horizons other than a histic, mollic, ochric, takyric, umbric, yermic, salic, or sulfuric horizon.

Distribution of Fluvisols (rough estimation supplied by soilgrids)

 

Reference soil MY054: Fluvisols

A well developed rubefied leached soil in subrecent beach deposits, 4 m above high tide level, with almost flat relief (slope 0-2 %), derived from adamellite (biotite granite and granodiorite) with some admixture from metamorphic rocks and sandstones. The groundwater table is within 200 cm and may have formed irregularly spaced large blotches of paler and darker coloured material in B3C horizon that has a sloping boundary to B2 horizon. Due to animal activity, there are blotches of dark A1 material in A2 horizon. The soils of the Sematan series are very poor and deficient in all major nutrients and need to be heavily fertilized if used for agriculture. (additional climatic data: days with precipitation >0.1 mm)

 

Classification

WRB 2014 
Fluvisol 
FAO-UNESCO-ISRIC 1974 
Dystric Fluvisol  
  
 

 

Local classification:Sematan series