Reference soil Kenya 21: Solonchak

KE021

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.

Distribution of Solonchaks (rough estimation supplied by soilgrids)

 

Reference soil KE021: Solonchaks

A salt-affected soil, dominated by quartz and clay minerals, derived from quaternary lacustrine sediments ("Chalbi beds") with cracks (extending to 1-2 cm width) to 20 cm depth and a very hard saline crust in dry season (many crystal needles).

 

Classification

WRB 2006WRB 1998
Gypsic-Puffic- Solonchak (Sodic Chloridic Takyric)Gypsi-Sodic- Solonchak (Takyric Chloridic)
0-100 cmsalic horizon
35-100 cmgypsic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Takyri-Sodic SolonchakTakyric Solonchak
0-20 cmochric A horizon
-salic
-sodic
0-20 cmochric A horizon
-high salinity
-takyric features