Reference soil Indonesia 32: Ferralsol

ID032

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 ID032: Ferralsols

CLASSIFICATION: The soil has all the properties for a Ferralic B horizon, except for the silt/clay ratio, which is slightly too high -> the required silt/clay of <0.2 is waived. LOCATION: The Indonesian monolith number is Jambi01. Site ID032 is located in the same area as Tropsoil sites Kuamang Guning (pedon Indonesia 6) and Kumang Guning unit 18 (pedon Indonesia 7). LAND USE AND VEGETATION: ID032 is comparable to ID033. Land use of ID032 is arable farming, while ID033 has still a secondary forest cover. The land clearing for the Kuamang Guning area started 5 years ago. ID032 is located in the "land clearing" experimental site with the treatment manual clearing, cover crop and coconut. Under permanent vegetation cover no or slight erosion. When cultivated with annual crops the soil is sensitive for sheet and rill erosion. Cassave is a major crop in the area. Other crops cultivated are upland rice, soybean, maize (poor stand), banana, coffee, coconut, jackfruit (Artocarpus integra). ADDITIONAL NOTES ON PROFILE DESCRIPTION: Shiny surfaces/cutans? are visible in porechannels and on surfaces of macro structures. Few yellowish coloured spots/pockets are present from 103 to 220cm, probably weathered C material. The dark red mottled deeper subsoil horizon -approximate parallel to the surface- can be frequently observed in deep roadcuts of rolling interfluves. Probably of pedegenetic origin as its boundary is approximate parallel to the surface.

 

Classification

WRB 2006 
Acric- Ferralsol (Alumic Clayic Xanthic) 
11-160 cmferralic horizon
 
11-160 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Haplic AcrisolDystric Nitosol
0-30 cmochric A horizon
11-103 cmalbic E horizon
0-30 cmochric A horizon
11-103 cmargillic B horizon

 

Local classification:Oksisol Haplik