Reference soil Indonesia 20: Ferralsol

ID020

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 ID020: Ferralsols

CLASSIFICATION: The soil was classified as Ferralsol/Oxisol in the field, but the analytical data indicate that the silt-clay ratio, and the CEC of the clay, are too high for the ferralic B or the oxic horizon respectively. The B horizon is cambic. SLOPE: 6-13%, 250-500m long. DEPTH LOWER GROUND WATER LEVEL: >120 cm. FLOODING: frequently flooded by rainwater. RISK OF EROSION: burning. VEGETATION: ferns, alang-alang & Kebun pinus. No lianes or saplings. ADDITIONAL NOTES ON PROFILE DESCRIPTION: AB - Also many very fine roots. Bw - Also few very fine roots. BCg - Also 2.5YR5/8. Cg1 - Also 2.5Y8/6 and 2.5Y8/3. Cg2 - Also 2.5Y8/3 and 2.5YR5/8.

 

Classification

WRB 2006 
Haplic- Ferralsol (Alumic Xanthic) 
5-55 cmferralic horizon
-reducing conditions
-stagnic colour pattern
 
5-55 cmferralic horizon
-reducing conditions
-stagnic colour pattern
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Ferralic CambisolXanthic Ferralsol
0-20 cmochric A horizon
5-75 cmcambic B horizon
-ferralic
0-20 cmochric A horizon
5-55 cmoxic B horizon
-ferralic