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classification of upper slope soils of a toposequence for rainfed ...

classification of upper slope soils of a toposequence for rainfed ...

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Detai led soi I and land maps <strong>of</strong> an area approximately 32.592ha, along a representative<br />

topographic location in the University <strong>of</strong> Agriculture, Abeokuta were produced <strong>for</strong> effective<br />

land use planning.<br />

The site is underlain by basement complex rock with quartz, schists, coarse grained and fined<br />

grained and gneissis as parent material. Three (3) soil series were identified with soil<br />

properties varying within short distance. Soil textural class ranges from sandyloam to sandy<br />

clayloam with parent gravel ranging from 0.8 - 76.3<br />

Soil reaction is slightly acidic to strong acid (PH 5.46 - 6.32) with moderate to high<br />

phosphorus (10.41 - 57.77)mg/kg and high base saturation (77.95 - n94.34)%. The<br />

coefficient <strong>of</strong> variability <strong>for</strong> soil properties ranging from (1.10 - 37.75%) with 18.71% foe<br />

available phosphorus, 16.34 <strong>for</strong> Ca++ and 37.75 <strong>for</strong> % gravel, 9.07 % <strong>for</strong> %OC, 9.48% organic<br />

matter, j.41<br />

<strong>for</strong> % base saturation<br />

Soil productivity indices <strong>for</strong> <strong>rainfed</strong> arable crops (yam, cassava and maize were developed <strong>for</strong><br />

the three (3) soil series (Alfisol) in the area. It involved ratings <strong>of</strong> relevant soil characteristics<br />

and using the ratings to calculate soil productivity index and soil fertility index. Actual<br />

productivity index (p) is the product <strong>of</strong> the rating <strong>for</strong> soil depth (d), texture (t), <strong>slope</strong>s (s), soil<br />

fertility index (f) and annual rainfall (w). The soil fertility index (f) is the product <strong>of</strong> rating<br />

<strong>for</strong> nutrients (Pn), organic matter ( I' ), base saturation (n), nature <strong>of</strong> clay minerals (e) and<br />

mineral reserve (m). Potential productivity index (PI) is the product <strong>of</strong> soil depth (d), texture

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