Reference soil Kenya 19: Planosol
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.
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.