Reference soil India 07: Luvisol

IN007

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 IN007: Luvisols

A deep, red loamy soil derived from granite gneiss (with quartz, feldspar, mica, and iron-coated quartz) in an undulating midland (slope gradients 3-5 %). The B horizon has a gravelly texture and contains quartz fragments of different size (2-50 mm) and shape. Soil reaction is neutral. REFERENCES: (1) Channasandra Series. In: Soil Series of India. (Eds. S. Lal, S.B. Deshpande & J. Seghal. 1994), pp. 177-180. National Bureau of Soil Survey and Land Use Planning, Nagpur. (2) Channasandra Series. In: Benchmark Soils of India - Morphology, characteristics and classification for resource management. (Eds. R.S. Murthy, L.R. Hirekerur, S.B. Deshpande & B.V. Venkata Rao. 1982), pp. 296-299. National Bureau of Soil Survey and Land Use Planning, Nagpur.

 

Classification

WRB 2014 
Luvisol 
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Pachi-Chromic LuvisolEutric Nitosol
- cmargic B horizon
- cmochric A horizon
- cmargillic B horizon
- cmochric A horizon

 

Local classification:Channasandra sandy clay loam