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Root growth of soybean (Glycine max L. Merr.) and cowpea (Vigna unguiculata Walp.) on a hydromorphic toposequence in Western Nigeria

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The effects of variations in edaphic and hydrologic factors over a short distance on the root growth of soybean cv. Hernon 237 and cowpea cv. IT 82 E-60 were studied in a hydromorphic toposequence. During the growing season the water table (WT) fluctuated from 0.43 to 0.94 m (high), 0.60 to 1.12 m (medium) and 0.72 to 1.51 m (low), respectively in 1983 and from 0.47 to 0.84 m (high), 0.63 to 1.13 m (medium) and 0.83 to 1 20m (low). respectively, in 1984. Poor soil aeration did not limit growth, even for high WT. Root penetration into the deeper soil was prevented at the low and medium water table sites by the presence of a naturally occurring compacted gravel layer at the 0.30-0.40 m depth. The absence of this layer at the high water table site resulted in root growth and proliferation of soybean roots even within the capillary fringe zone immediately above the water table. Cowpea roots, however, were not observed in this saturated soil zone. Cowpea roots penetrated deeper in high than in medium and low WT. Evapotranspiration (Et) and Et/Eo values of both crops were significantly greater at the high than at medium or low water table.

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Plant and Soil

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