Institutes

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Institutes

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Browsing Institutes by Author "Ojo-Atere, J. O."

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    Characteristics and Classification of Some Upper Slope Soils in Savanna Ecosystems of South Western Nigerian
    (Faculty of Agriculture, University of Ife, 1983) Ojo-Atere, J. O.; Oladimeji, M. O.
    Some upper slope soils of the savanna ecosystems of southwestern Nigeria were studied with a view to broaden their data base and pave the way for a better classification of the soils. The three profiles used were obtained from Shaki, Igbeti and Babaade in the northern part of Oyo State. The soils were subjected to physical, chemical, mineralogical and micromorphological analyses. Generally, it was observed that the morphological and chemical characteristics of the soils studied have been affected considerably by the interaction of climate, parent material, relief, vegetation, time and biological factors. The physical, chemical and mineralogical data do not show any well-defined sequence in the profiles. These analytical data indicate that the surface horizons may be developed in transported material, while the subsurface horizons may be derived from the underlying rock. These indicate the complexity of the profiles and also confirm the non-uniformity of the parent materials. Clay mineralogy indicates that Kaolinite is dominant in the soils, with considerable amounts of smectite and mica. Cutans were associated with both Inceptisols and Alfisols in the soils studied. Thus, cutah may not be a good diagnostic feature for argillic horizons in south western Nigeria.
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    Micromorphology and Soil Formation of Some Savanna Alfisols in South Western Nigeria
    (Faculty of Agriculture, University of Ife, 1984) Ojo-Atere, J. O.
    The relationship between micromorphology and soil formation in some well-drained soils in the savanna ecosystem of south-Western Nigeria was studied. Arrangements of soil constituents were evaluated in nineteen (75 x 251nm) thin sections made from undisturbed samples. Thin section studies show that the related distribution of plasma and skeleton grains is usually agglomeroplasmic with some intertextic patches in the surfacial horizons of the soils. The sub-surfacial horizons of the soils are characterized by a porphyroskelic related distribution. Pedological features are glaehules and cutans. Pedorelicts and Ldthorelicts were recognized: The sub-rounded shape of the pedoreticts indicates that they have been transported and the presence of the nodules in the surfacial horizons of most profiles probably shows former soil process.