Reference soil Kenya 19: Planosol

KE019

Planosols occur in level landscapes throughout the world often associated with broad river valleys.

Characteristics

Soils having an eluvial horizon, the lower boundary of which is marked. within 100 cm from the soil surface, by an abrupt textural change associated with stagnic properties above that boundary. The feature of albeluvic tonguing, however, is lacking.

Distribution of Planosols (rough estimation supplied by soilgrids)

 

Reference soil KE019: Planosols

LOCATION: KE 19 is located in a plain close to a termite mound, but out of its influence. KE 18 is located on the slope of the mound and KE 17 on its active part. MICRO RELIEF: termite mounds of 1-2 m high and a diameter of 3-6 m occur at distances of 30-50 m. VEGETATION/LAND USE: on the mounds shrubs, between the mounds grass, which is used for extensive grazing. SOIL PROCESSES: profiles KE 17, 18 and 19 are associated soils. Termites have throroughly mixed the different horizons as occuring in profile KE 19 which results in KE 17. KE 18 is a transition to KE 19. Additional notes on profile description: Ah, E1 and E2: mottles are dark yellowish brown; Bt2: few weak not intersecting slickensides; texture: gravelly and stony clay; stones are mainly quartzitic with a few jaspis and weathering granites; mottles are reddish yellow; BC: mottles are yellowish brown and white.

 

Classification

WRB 2006WRB 1998
Alic- Planosol (Albic Hyposodic Clayic)Ali-Hyposodic- Planosol (Albic)
12-50 cmalbic horizon
50-105 cmargic horizon
-abrupt textural change
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Ali-Dystric Planosol sodicSolodic Planosol
0-12 cmochric A horizon
12-50 cmalbic E horizon
50-105 cmargic B horizon
-abrupt textural change
-stagnic
0-12 cmochric A horizon
12-50 cmalbic E horizon
50-105 cmargillic B horizon
-abrupt textural change
-hydromorphic