Reference soil Zimbabwe 12: Lixisol

ZW012

Lixisols occur dominantly in the drier parts of the tropics and subtropics. Their high base status is partly due to less leaching, partly to admixture from airborne dust from adjacent desert regions.

Characteristics

Soils having an argic horizon (a subsurface horizon with a distinct higher clay content than the overlying horizon), which has a cation exchange capacity of less than 24 cmolc per kg in some part, either starting within either: 100 cm from the soil surface, or 200 cm from the soil surface if the argic horizon is overlain by loamy sand or coarser textures throughout. They have a base saturation (total amount of Ca, Mg, K and Na with respect to the cation exchange capacity) of 50 percent or more in the major part between 25 and 100 cm from the soil surface.

Distribution of Lixisols (rough estimation supplied by soilgrids)

 

Reference soil ZW012: Lixisols

(1) Natural vegetation consists predominantly of medium-sized open woodland trees and shrubs. Brachystegia spiciformis and Julbernardia globiflora trees and shrubs dominate, but there are now more common Terminalia sericea and Parinari curatellifolia trees and shrubs. Vegetation samples were collected from the immediate area outside the fenced Trial Block, and await full identification. (2) Only a few grasses and arable weeds were observed in the immediate vicinity of the pit. (3) The land has been cleared and stumped, to accomodate the ICRAF Agroforestry Trial Block. The upper part of the Block, on the edge of which the pit is situated, was cleared in 1990. The land was ploughed and agroforestry shrubs were planted in December 1990. At the time of planting, each shrub received 10 litres of water every two weeks for a two-month period. Thereafter, no water was applied and the shrubs had to rely on the seasonal rainfall, falling during the months of November to April. During the 1990/91 season, 251 mm

 

Classification

WRB 2006 
Haplic- Lixisol (Albic Epidystric Profondic Arenic) 
24-132 cmalbic horizon
 
24-132 cmalbic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Dystri-Albic ArenosolAlbic Arenosol
0-24 cmochric A horizon
24-132 cmalbic E horizon
0-24 cmochric A horizon
24-132 cmalbic E horizon