Reference soil Kenya 22: Solonetz

KE022

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 KE022: Solonetz

A salinic soil derived from quaternary sediments ("Hedad beds") with very light seasonal use (depressions devoid of vegetation), biological activities (krotowinas). There are few fine black primary mineral fragments throughout the profile. vegetation: accacia reficiens, indigofera Spinosa

 

Classification

WRB 2006WRB 1998
Haplic- Solonetz (Abruptic)Haplic- Solonetz
32-170 cmargic horizon
55-90 cmnatric horizon
-abrupt textural change
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic SolonetzOrthic Solonetz
0-8 cmochric A horizon
32-170 cmargic B horizon
55-90 cmnatric B horizon
-abrupt textural change
0-8 cmochric A horizon
32-170 cmargillic B horizon
55-90 cmnatric B horizon
-abrupt textural change