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

✍ Scribed by D. Siriri; M. M. Tenywa; T. Raussen; J. K. Zake

• Publisher: John Wiley and Sons
• Year: 2005
• Tongue: English
• Weight: 252 KB
• Volume: 16
• Category: Article
• ISSN: 1085-3278
• DOI: 10.1002/ldr.688

✦ Synopsis

Abstract

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 11 g 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 © 2005 John Wiley & Sons, Ltd.