Although rill and gully erosions in Zimbabwe are under control, sheet erosion is still a problem, with estimated rates of soil loss of 50 to 80 t/ha/year. Discusses development of the SLEMSA model building framework, to predict sheet erosion losses, from arable lands in areas of high intensity rainfall. Within the physical systems of (crops, climate soil, topography). There are control variables
... [Show full abstract] for modelling purposes. These include rainfall energy/interception soil erodibility, slope steepness/length. The resulting sub-models are then combined to give a bed estimate of mean annual soil loss. The purpose of the soil life-span model is to provide a measure of the consequences of an existing soil loss rate. Presents an example application of this model to a communal area, noting the benefits of crop ridges on contoured land. (C.J.U.)