Reference soil Indonesia 03: Luvisol

ID003

Luvisols occur mainly in temperate regions, particularly in areas with a Mediterranean-type of climate.

Characteristics

Soils having an argic horizon (a subsurface horizon with a distinct higher clay content than the overlying horizon) with a cation exchange capacity equal to or more than 24 cmolc per kg clay throughout.

Distribution of Luvisols (rough estimation supplied by soilgrids)

 

Reference soil ID003: Luvisols

PHYSIOGRAPHY: Lower slope of Gunung Pangrango volcanic cone. PARENT MATERIAL: Intermediate (andesitic) volcanic ash (0-69 cm) over volcanic tuff with approximately 20% andesite gravel. Thelatter parent material consists of two ash deposits (69-85 and 85-125+ cm), which is marked by the occurence of a weakly developed 3Ah-horizon. LAND USE AND VEGETATION: Tea estate. Whole area is cleared of its original vegetation, the more remote places being covered with secondary shrubs and trees. REFERENCES: - P. Buurman et al, 1980: "Red soils in Indonesia", pp. 24-47; Pudoc, Wageningen.

 

Classification

WRB 2006 
Andic-Cutanic- Luvisol (Ruptic Humic Epidystric) 
0-69 cmumbric horizon
44-69 cmargic horizon
69-150 cmcambic horizon
-andic
-lithological discontinuity
 
0-69 cmumbric horizon
44-69 cmargic horizon
69-150 cmcambic horizon
-andic
-lithological discontinuity
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Andi-Humic AlisolOrthic Luvisol
0-69 cmumbric A horizon
44-69 cmargic B horizon
69-150 cmcambic B horizon
-andic
-weatherable minerals
0-69 cmumbric A horizon
44-69 cmargillic B horizon
69-150 cmcambic B horizon
-exchange complex dominated by amorphous material

 

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