Reference soil Zimbabwe 02: Ferralsol
Ferralsols occur in tropical and subtropical regions of the world, mainly on old and stable land surfaces.
Characteristics
Soils having a ferralic horizon (strongly weathered horizon with low-activity clays and very low amounts of weatherable minerals) between 25 and 200 cm from the soil surface. They lack a nitic horizon (a horizon with strongly developed, nut-shaped structure) and do not have a layer which fulfils the requirements of an argic horizon and which has, in the upper 30 cm, 10 percent or more water-dispersible clay.
Reference soil ZW002: Ferralsols
(1)The site would normally be under natural woodland, dominated by Julbernardia globiflora, Parinara curatellifolia and Uapaca kirkiana. This woodland has been cleared by the local population, and grasses and shrubs have regrown. The main grass species is Hyperthelia dissoluta, with some Aristida meridionalis. The shrub species include Uapaca kirkiana, Tephrosia rhodesica, Rhynchosia resinosa, Strynos spinosa, Acacia nilotica, Julbernardia globiflora (dominant), Lantana camara, Dichrostacys cinerea, Parinara curatell- ifolia and Clerodendrum glabrum. In addition, a number of herbaceous species were identified - Tagetes minuta, Blumea crispata and Vernonia glabra, Trichodesma physaloides and Aspilia pluriseta. (2)A nearby stand of Eucalyptus regrowth was observed. (3)Evidence of fire burns in the vicinity of the pit were observed. (4)Area has been lightly grazed by a small herd of cattle. (5)A road drainage cutting is situated about 5 m from the pit, and was constructed in 1988, when the road past Epworth Mission Station was sealed. (6)Lister (1986,p.82) indicates that the Epworth area is situated on the African Erosion Surface, and that the regularly jointed granite boulders and balancing rocks are residua from the Post-Gondwana Erosion Surface. (7)The pit terminates at about 160 cms onto many, coarse to very coarse, moderately weathered, granite boulders. (8)Horizon 7 has been designated Cw because of the observed presence of remnant rock structures, although there is little evidence of actual rock fragments. (9)Under the headings of biological activity, the following comments must be made: in Horizons 1 and 2, termite and ant channels were observed; in Horizons 3 and 4, krotovinas of varying dimensions were noted and in addition, plant root channels stained black as a result of the decomposition of the root material; in Horizons 5 and 6, similar darkened channels from decomposed roots were observed; no biological activity was recorded in Horizon 7. (10)A number of insect specimens were taken for identification. Two beetle (Coleoptera) specimens included (Tenebrionidae Opatrinae) Anomalipus mustela and (Carabidae Graphopterinae) Piezia mashuna. Two ant specimens included (Formicidae Ponerinae) Paltothyreus tarsatus, (Formicidae Myrmicinae) Tetramonium sp, and the one termite (Isoptera) specimen could not be identified adequately.