Crop and soil variability on terraces in the highlands of SW Uganda

Terrace benches on the hillslopes of Western Uganda exhibit a crop-yield gradient: upper portions of terraces produce less than the lower sections. We investigated the soil factors responsible for this yield variation on 30 terraces along 5 toposequences in what was predominantly a Ferralsol. Two levels of spatial analysis were conducted: (1) variation within individual terraces; and (2) differences across hill-slope positions. A greenhouse experiment further examined this fertility gradient using soils extracted from the upper, middle and lower parts of the terrace. This included a nitrogen (N) treatment of 70 mg N kg(-1) soil. In the fields sorghum (Sorghum bicolor) grain yield differed significantly (p:<= 0.05) across terraces, increasing from 0.4 Mg ha(-1) on the upper 40 per cent of terrace to 2.5 Mg ha(-1) on the lower 40 per cent. Soil bulk density decreased down the terraces from 1.41 g cm(-3) to 1.18 g cm(-3), causing an increase of hydraulic conductivity from 1.6 cm h(-1) to 7.3 cm h(-1), from the upper to the lower part, respectively. Organic carbon (C) and total N increased from upper to lower terrace sections. In the greenhouse, sorghum growing on soils from which the soil physical limitations have been removed did not show significant yield differences across a terrace as observed in the field. Response to N was most pronounced on the upper terrace sections, increasing sorghum dry matter from 3 g pot(-1) to 15 g pot(-1). On the lower terrace, N amendment increased dry matter from 4 g pot(-1) to 11g pot(-1) Technologies to improve the adverse soil physical conditions and the N limitations on upper terrace parts while preventing tillage- and soil-erosion-induced terrace scouring are required. Copyright (c) 2005 John Wiley & Sons, Ltd.