Sustainable crop production requires a correct understanding of the characteristics of
soils on a landscape, which helps to curb the incidence of wrong generalization in
soil use and management practices. This study was carried out to assess the mineral
composition and physicochemical properties of soils at different positions along the
toposequence of a shale-derived soil at Amaeke, Abia State. The experiment was laid
out in a Randomised Complete Block Design involving topounit as treatment and of
five (5) levels (crest, upper slope, middle slope, lower slope and valley bottom) with
three (3) replicates each of disturbed and undisturbed soil samples randomly
collected from each topounit to give a total of fifteen (15) observational units. The soil
samples were processed and analzsed in a laboratory. Data obtained were subjected
to analysis of variance using Genstat analytical software, while significant means
were separated using Fisher’s Least Significant Difference at a 5% probability level.
The results showed that the topounits had similar mineral composition and rating
except the crest which in addition to other common minerals, contained hematite and
goethite. The crest was highest in bulk density (1.71 mg / m3), clay flocculation index
(79.94%), and mean weight diameter (6.11 mm), but lowest in sand content (41.61%),
and the upper slope was highest in available water capacity (30.31%). The valley
bottom was highest in available phosphorus (30.02 mg/kg), organic carbon (1.32%),
total exchangeable bases (16.68 cmol / kg) and extractible iron (0.42 mg/kg), at the
same time, the middle slope was highest in exchangeable potassium (0.29 cmol / kg).
The topounits varied in the physicochemical properties in such a way that soil
structural stability indices and chemical properties decreased and increased,
respectively, along the descending part of the slope.
Keywords: Topounits, toposequence, bulk density, organic carbon, crest, valley
bottom
