Reference soil Malaysia 61: Arenosol

MY061

Arenosols occur over large areas in Africa, central and western Australia, the Middle East and central China. Smaller areas are found along coastlines all over the world.

Characteristics

Soils with a loamy sand or coarser texture either to a depth of at least 100 cm from the soil surface, or to a (petro-)plinthic or salic horizon between 50 and 100 cm from the soil surface. They contain less than 35 percent (by volume) rock fragments or other coarse fragments within 100 cm from the soil surface and have no diagnostic horizons other than an ochric, yermic or albic horizon, a (petro-)plinthic or salic horizon below 50 cm from the soil surface, or an argic or spodic horizon below 200 cm below the soil surface.

Distribution of Arenosols (rough estimation supplied by soilgrids)

 

Reference soil MY061: Arenosols

A recent alluvial soil on gentle slope landinwards, near swale separating two ridges. There are common mottles of different colours between 15 and 122 cm. In Bs horizon there are common reddish brown concretions, often with a layer of more reddish material (iron oxide ?) surrounding it. This material is concentrated at 46-60 cm, from 60-76 cm it is less dark and more like mottles. Most roots do not grow deeper than 46 cm. The 2C horizon consists of coarser sand and is distinctly micaceous. The soils of the Rambungan series are good for coconut but would need adequate amounts of fertilizer for obtaining good yields. Melons are also planted with success. (additional climatic data: days with precipitation >0,1mm)

 

Classification

WRB 2014 
Arenosol 
FAO-UNESCO-ISRIC 1974 
Cambic Arenosol  
  
 

 

Local classification:Rambungan series