Reference soil Kenya 65: Solonetz

KE065

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 KE065: Solonetz

Faint bleached grains in the E-horizon. Slides: 10,234 - 10,237.

 

Classification

WRB 2006WRB 1998
Mollic-Stagnic-Vertic- Solonetz (Abruptic Clayic)Molli-Vertic- Solonetz (calcic horizon Stagnic)
0-38 cmmollic horizon
38-72 cmvertic horizon
38-97 cmnatric horizon
-abrupt textural change
-vertic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Calci-Mollic SolonetzSolodic Planosol
0-38 cmmollic A horizon
38-97 cmnatric B horizon
-abrupt textural change
-soft powdery lime
-stagnic
0-38 cmmollic A horizon
38-97 cmnatric B horizon
-soft powdery lime