Reference soil India 03: Acrisol
Acrisols occur dominantly in the wetter parts of the tropics and subtropics and the warm temperate regions in relatively young landscapes.
Characteristics
Soils having an argic horizon (a subsurface horizon with distinct higher clay content than the overlying horizon), which has a cation exchange capacity of less than 24 cmolc per kg in some part, either starting within 100 cm from the soil surface, or within 200 cm from the soil surface if the argic horizon is overlain by loamy sand or coarser textures throughout. They have a base saturation (total amount of Ca, Mg, K and Na with respect to the cation exchange capacity) of less than 50 percent in the major part between 25 and 100 cm from the soil surface
Reference soil IN003: Acrisols
A deep, moderately well drained, red and yellow loamy soil on a plateau with slopes varying between 1 and 3 %. Clay content increases with depth and the soil shows decreasing permeability in the lower horizons. Soil reaction is strongly acid. The lower part shows common yellowish red to red mottles. Strong biological activity is noted in the upper 70 cm. The land is hardly affected by erosion. SOIL MORPHOLOGY: second colour Bt1 10YR 5/2, second colour Bt2 10YR 5/2, second colour Bt3 10YR 7/1, all moist.