Reference soil India 04: Solonchak
Solonchaks occur where saline groundwater comes near to the surface, or where through evapo(transpi)ration salts from the soil water accumulate in the soil, e.g. in desert regions
Characteristics
Soils having a salic horizon (horizon with accumulation of salts more soluble than gypsum) within 50 cm of the soil surface. They have no diagnostic horizons other than a histic, mollic, ochric, takyric, yermic, calcic, cambic, duric, gypsic or vertic horizon.
Reference soil IN004: Solonchaks
A deep, poorly drained, grayish coloured saline soil with a silty loam texture, developed in deltaic alluvium in the western part of the Ganges delta. The topsoil is massive, caused by puddling. The soil has a neutral to slightly alkaline reaction, mottles and rusty specks, iron concretions below 22 cm and very small mica flakes throughout. MORPHOLOGICAL DESCRIPTION : AB slightly firm. Bg2 mottled: 2.5Y 5/0, 5Y 4/4, 10YR 5/4. Apg and ABg moderately permeable, Bg1 and Bg2 slowly permeable.