Reference soil Indonesia 22: Ferralsol

ID022

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 ID022: Ferralsols

CLASSIFICATION: The upper 33 cm constitute a young cover of weathered andesitic ash, overlying strongly weathered tuff deposits (33-75 cm, and 75+ cm) of the old Geureudong volcanic system. The AB, Bw, 2Bw and the 3Bw horizons have a low CEC and ECEC and are classified as ferralic B and oxic horizon respectively, although the content of weatherable minerals in the sand fraction are slightly too high. If the latter is taken into account, the soil should be classified as Ferric Cambisol and Oxic Humitropept respectively. LAND USE AND VEGETATION: Ladang (shifting cultivation), infrequently burned. Presently long fallow bush land. Remnants of primary forest in valleys and at remote places. ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ah - also many fine and very fine roots. AB - also many fine and very fine pores ; also many fine and very fine roots. Bw - also many very fine pores ; also common fine and very fine roots. 2Bw - also common very fine roots.

 

Classification

WRB 2006 
Haplic- Ferralsol (Alumic Ruptic Clayic) 
17-75 cmferralic horizon
-lithological discontinuity
 
17-75 cmferralic horizon
-lithological discontinuity
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Dystri-Ferralic CambisolOrthic Ferralsol
0-17 cmochric A horizon
17-75 cmcambic B horizon
-ferralic
0-17 cmochric A horizon
17-75 cmoxic B horizon

 

Local classification:Oksisol Humik (PPT-Bogor 1981)