Reference soil India 06: Luvisol
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.
Reference soil IN006: Luvisols
A deep, well drained, yellowish red soil with a subangular blocky structure and a stone line at 60-70 cm depth. The surface horizon has a slightly gravelly sandy loam texture, overlying a slightly gravelly sandy clay loam. Below the stone line a gravelly sandy clay to clay occurs with parts of weathered parent material, increasing in amount with depth. LOCATION: profile is located next to the South India Carbonic Gas Industries. MICROMORPHOLOGY: thin sections show many clay skins between 19 and 34 cm, abundant clay skins between 37 and 52 cm, and few clay skins between 86 and 101 cm depth. NATURAL VEGETATION: Lantana camera, Pongamea glabra, Tamarindus indica, Croton sparsiflorus and grasses. CROPS: "ragi" (Eleusinea coracano), "jowar" (Sorghum vulgare), "avare" (Dolichos lal lab) and "niger" (Guizotia abyssinica). PERMEABILITY: moderately rapid. MORPHOLOGY: an oblique stone line of partly weathered diorite occurs between 58 and 73 cm.