Reference soil Indonesia 35: Ferralsol

ID035

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 ID035: Ferralsols

LOCATION: The indonesian monolith number is SUMBAR02. The site is comparable to TROPSOIL profile Indonesia2. EROSION: At about 400m from the site are erosion test plots. From 3 years of testing the following average erosion rates have been calculated: - control plot (bare soil) = 300 ton/ha - vegetation contour strips= 25 ton/ha - contour ridges = 20 ton/ha - terraces = 1 ton/ha Note that the data are averages over several years and there are several variations on each technique used. Lime has been used, although quantity and number of applications are not known(verbal information). ADDITIONAL NOTES ON PROFILE DESCRIPTION: A few clear quartz grains are visible throughout the profile. The stickiness and plasticity varies considerably within a narrow moisture range; from sticky and plastic to slightly sticky and slightly plastic. Penetrometer reading: Ap1 1, Ap2 4 to 4.5, all B horizons around 2 kg/cm2.

 

Classification

WRB 2006 
Vetic- Ferralsol (Alumic Clayic Xanthic) 
21-160 cmferralic horizon
 
21-160 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Xanthic FerralsolXanthic Ferralsol
0-21 cmochric A horizon
21-160 cmferralic B horizon
0-21 cmochric A horizon
21-160 cmoxic B horizon

 

Local classification:Oksisol Haplik