Reference soil Indonesia 17: Luvisol

ID017

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 ID017: Luvisols

ADDITIONAL NOTES ON PROFILE DESCRIPTION: A1 - Also black colour (N2/0); also many medium and few coarse roots. B2 - Also many medium and few coarse roots. C - Colour mixed with 10YR4/4; also common medium and few coarse roots. A1b - Also common medium and few coarse roots. B1b - Also common medium and few coarse roots. B2b - Also 5YR5/8. B3 - Also 10YR5/4 and 2.5Y6/5 ; stones and gravels are strongly calcareous. R - white coloured rock. REFERENCES: - Hommel, P.W.F.M., 1987. Landscape-Ecology of Ujung Kulon (West Java, Indonesia). Soil Survey Institute, Wageningen, The Netherlands.

 

Classification

WRB 2006 
Haplic- Luvisol (Ruptic Clayic Novic) 
39-105 cmargic horizon
-lithological discontinuity
 
39-105 cmargic horizon
-lithological discontinuity
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic LuvisolOrthic Luvisol
0-7 cmochric A horizon
39-105 cmargic B horizon
0-7 cmochric A horizon
39-105 cmargillic B horizon