Reference soil Indonesia 04: Ferralsol

ID004

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 ID004: Ferralsols

CLASSIFICATION: Though having low bulk densities throughout, the soil doesn't meet the requirements of an Andosol (Andept) because its exchange complex is insufficiently made up of amorphous materials. Instead, the clay fraction has ferralic properties. PHYSIOGRAPHY: Flat to slightly undulating dissected footslope of Gunung Pangrango volcano. PARENT MATERIAL: Intermediate (andesitic) volcanic tuff. LAND USE AND VEGETATION: Rainfed arable farming. Cassava plot. Poor stand, probably due to Mn concretion layer. Untill recently the supply of irrigation water was sufficient to grow wet landrice. Whole area is cleared of its original vegetation. ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ap: many termite nests (2 per meter, up to 10 cm in diameter). Bw: many vertical channels filled with light coloured top soil material. REFERENCES: - P. Buurman et al, 1980: "Red soils in Indonesia", pp. 24-47; Pudoc, Wageningen.

 

Classification

WRB 2006 
Gibbsic- Ferralsol (Manganiferric Dystric Clayic) 
26-170 cmferralic horizon
26-80 cmferric horizon
 
26-170 cmferralic horizon
26-80 cmferric horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Dystri-Haplic FerralsolOrthic Ferralsol
0-26 cmochric A horizon
26-170 cmferralic B horizon
-ferric
0-26 cmochric A horizon
26-170 cmoxic B horizon
-ferric

 

Local classification:Kambisol Oksik (PPT-Bogor, 1981)