| dc.description.abstract |
Engineering geological and geophysical investigation were carried out at Alagbaka extension of
Akure, Ondo State with the aim of assessing the characteristics of the subsoil in order to identify
competent zone that would support any proposed structures in the area. The study area is presently
undergoing developmental projects such as erection of buildings of different designs and
telecommunication mast. The need for both engineering geological and geophysical investigation of
the subsoil became imperative. A variety of twenty six disturbed soil samples were collected from
different pits at a depth of about 2m. The samples were analyzed for natural moisture content, grain
size analysis, Atterberg limits, standard compaction, unconfined compressive strength and
consolidation tests. The Schlumberger configuration was carried out for data acquisition, the halfcurrent
electrode (AB/2) was used and the quantitative interpretation of the vertical electrical
sounding (VES) data which involved partial curve matching and computer iteration. A total of
twenty six soundings were occupied across the study area and geo-electrical section were
constructed across the geology of the study area. A model using Consolidation, Atterberg limits,
Unconfined compressive strength, Resistivity value at 2m, and Resistivity of the bedrock (CAURR)
approach was introduced in decision making. The results of the laboratory tests reveals that moisture
content range from 6.1% to 18.5%, liquid limit from 25.1% to 48.6%, plastic limit from 17.6% to
29.5%, linear shrinkage from 2.9% to 7.7%, and plasticity index from 5.2% to 19.5%. The grain
size analysis showed that the amount of fines range from 20.6% to 47.4%. The specific gravity range
from 2.65 to 2.8, maximum dry density from 1820Kg/m3 to 1998Kg/m3 and optimum moisture
content from 13.2% to 19.7%. Coefficients of consolidation range from 0.02019 to 0.02944 and the
shear strength values varied from 74.1kPa to 103.8kPa. The geo-electrical section reveals a total of
four geo-electric layers which comprise of the top soil, weathered layer, partially weathered/partially
fractured bedrock and the fresh Basement. The superimposing of the competency map generated
from consolidation, Atterberg limits, unconfined compressive strength, resistivity and resistivity of
the bedrock parameters divided the study area into extremely high competent zone, very high
competent zone, high competent zone and moderately competent zone. Similarly, the CAURR
model classified the study area extremely high competent zone, very high competent zone, high
competent zone and moderately competent zone. It can be concluded from the study that the map
generated from superimposing the five competence parameters and the CAURR model generated
four similar zones in line with the previously established zonation. |
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