Reference soil Indonesia 19: Ferralsol

ID019

Ferralsols occur in tropical and subtropical regions of the world, mainly on old and stable land surfaces.

Characteristics

Soils having a ferralic horizon (strongly weathered horizon with low-activity clays and very low amounts of weatherable minerals) between 25 and 200 cm from the soil surface. They lack a nitic horizon (a horizon with strongly developed, nut-shaped structure) and do not have a layer which fulfils the requirements of an argic horizon and which has, in the upper 30 cm, 10 percent or more water-dispersible clay.

Distribution of Ferralsols (rough estimation supplied by soilgrids)

 

Reference soil ID019: Ferralsols

CLASSIFICATION: Although the material of the B horizon has a smeary consistence and a high phosphate retention, it does not meet the requirements of andic properties because the oxalate extractable Al and Fe is too low and the bulk density is too high. On account of the low CEC and ECEC, the B horizon is classified as ferralic. VEGETATION: Remnants of primary forest in valleys and at remote places.

 

Classification

WRB 2006 
Gibbsic- Ferralsol (Dystric Ruptic Clayic) 
29-110 cmferralic horizon
-lithological discontinuity
 
29-110 cmferralic horizon
-lithological discontinuity
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Veti-Xanthic FerralsolXanthic Ferralsol
0-29 cmochric A horizon
29-110 cmferralic B horizon
-smeary consistence
0-29 cmochric A horizon
29-110 cmoxic B horizon
-smeary consistence

 

Local classification:Latosol Oksik (PPT-Bogor 1981)