Reference soil Kenya 60: Solonetz

KE060

Solonetzes occur where a sodium source supplies the clay-rich subsoil with exchangeable Na, causing peptization of clay and organic substances and deterioration of the topsoil.

Characteristics

Soils having a natric horizon (a subsurface horizon with distinct higher clay content than the overlying horizon and more than 15% exchangeable sodium) within 100 cm from the soil surface.

Distribution of Solonetz (rough estimation supplied by soilgrids)

 

Reference soil KE060: Solonetz

Little soil fauna activity. Cracks from 39 to 80 cm. Slides: 10,195 - 10,196.

 

Classification

WRB 2006WRB 1998
calcic horizon- SolonetzOrthicalcic- Solonetz
30-110 cmcalcic horizon
5-70 cmargic horizon
70-110 cmnatric horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Calcic SolonetzOrthic Solonetz
0-16 cmochric A horizon
30-110 cmcalcic horizon
5-70 cmargic B horizon
70-110 cmnatric B horizon
-calcaric
-sodic
0-16 cmochric A horizon
30-110 cmcalcic horizon
5-70 cmargillic B horizon
70-110 cmnatric B horizon