Reference soil Kenya 13: Solonetz
KE013
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 KE013: Solonetz
A moderately well drained brown to yellowish brown soil with a moderately sodic subsoil and moderate surface sealing (3mm), derived from fine-grained sandstones and siltstones (Upper Maji-Ya-Chumvi beds). Below 35 cm mottles appear coloured strong brown, increasing with depth; termite mounds (4-7m diameter, 1,5 m height) exist. (R3 pg 253)