Reference soil Zimbabwe 01: Lixisol
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.
Reference soil ZW001: Lixisols
(1)Profile is located under grass/clover,adjacent to the Experimental Farm trials. (2)Grass identifications include Panicum repens, Heteropogon contortus, Eragrostis tenwifolium, Eragrostis pseudosclerantha, Digitaria ciliaris, Hyparrhenia filipendula, Chloris pychinothrix, Sporobolus pyramidalis, and Bothriochloa insculpta. The clover species is Trifolium. (3)A wide range of crops are grown in the Farm trials. During the wet summer season, maize, sunflower, soyabeans, groundnuts, sorghum, pearl and finger millets, potatoes, summer wheat, pulses, bambara nuts and cowpeas. During the dry winter season, winter wheat, winter barley and potatoes are grown. (4)There is evidence of termite activity, particularly in the upper horizons (0-30 cms). Covered channels, constructed by the insects since the pit was dug, extend down to 150 cms. A number of termite and ant fungal gardens were observed in the field examinations, and one large termite garden was collected for display purposes. (5)Common, small, white fungal colonies occur in the first horizon (0-27 cms). Two areas of expanding mycelia developed on the pit face at about 100 cms depth. (6)Many mites were observed on the profile face. In addition to these and the termites, colonies of small black ants and centipede insects were observed. (7)Field texturing reveals a somewhat inactive clay fraction. The presence of sand grains in the texturing was also observed - fine in the upper horizons, medium-sized in the middle horizons, and with coarse grains in the lower horizons. Texturing also reveals the evidence of water stable aggregates. The amount of these aggregates appears to decrease with depth from 27 - 160 cms. (8)Very rare fragments of weathered gabbro in the soil profile, which were generally yellowish brown/black/whitish in colour and between 3 - 5 mm. in size. (9)One small, (230 mm) subrounded boulder of gabbro was extracted from the pit. A skin of weathered gabbro surrounded the extracted core. (10)Very fine pores (<1 mm) were observed from 49 cms to depth. Some of these pores were caused by roots, which had since decomposed. (11)Slight colour variegations were noted from 47 cms to depth but were difficult to code. (12)Water permeability into peds of the upper horizons (0 - 27 cms) was slower than those of lower horizons, presumeably because of the presence of organic matter in the topsoils. (13)Iron/manganese stains were observable from 23 cms, became more numerous with depth, but also less prominent. (14)Under virgin conditions, the site would normally be located under Brachystegia spiciformis/Julbernardia globiflora woodland. These species, along with Uapaca kirkiana, Acacia sp. and Erithrina sp., presently occur in an undisturbed area of the adjacent Royal Harare Golf Course. Occasional large Brachystegia trees occur within the grounds of the Experimental Farm, one of which is 30 m from the pit. (15)Examination of the soil profile reveals the presence of shiny ped surfaces, which are recorded in the profile description as cutans on ped face