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ECOLOGICAL STUDIES ON TILE SYMBIOSIS OF TER ITOMYCES ...

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2el*2 SOILS<br />

The experimental sites around tlolcwa were at elevations between<br />

180-230 m. The general area van gently undulating with broad inter-<br />

fluvess and was occupied by soils of the Kulfo Association which are<br />

developed on coarse Nupe Sandstone (Valette 1973)o The association<br />

Is dominated by very deep, reddish soils with a sandy clay loam to<br />

clay texture in the subsoil. Moat of the soils are ferrisolsl with<br />

a sandy surface layer with low water-retention capacity. The soils<br />

in the experimental sites were a complex mosaic of the Kulfo Series<br />

(very deep, red sandy clay D horizon between 2511 and 6011) and the<br />

Dangappo Series (very deep red clay D horizon within 25") (Valette<br />

1979-<br />

At nabba the soils on the northern boundary of the forest were<br />

of the Rabba. Complex Association on an old alluvial sandy terrace*<br />

The main characteristics were deep to very deep brownish sands (Valette<br />

1973)e The forest was situated where the terrace descended to the<br />

floodplaine The forest *oil was hydromorphics developed on alluviuml<br />

with a dark Creyl weak crumb-structured topsoil (0-4ý5 cm) overlying a<br />

laroely structurelesel pale yellow-grey subsoile In the wet season<br />

the water table was at 50-150 cm (Wood et ale In press)*<br />

Analyzes of reprosentative profiles are given in Table 2,1,1,<br />

39.

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