Abstract
Due to incessant highway failures, the
mineralogy, geological and geotechnical properties and behavior of the
subgrades were investigated. Methods involved field sampling, geotechnical
laboratory and x-ray diffraction analysis. Results show a complex mineral
assemblage consisting of varying proportions of several clay and non-clay
minerals with a general prevalence in kaolinite (0.9 – 57.3%) and quartz (3.4 -
87.3%). One-fifth of the soils contain 2:1 expansive clay minerals of the
smectite (Na-montmorillonite) group, with at least 20% of each sample recording
10 – 30% of the expansive clay minerals in the failed highway sections. The
maximum range of the 2:1 expansive clay was 14.0 – 22.0cts with a mean range of
7.2 – 9.7cts and standard deviation varying from 7.0 to 7.9 across the
different rock terrains. The 2:1 expansive clay mineral of smectite group
depicted weak and low bearing strength characteristics (CBR range of 1.
09–3.0%) natural bulk density of 720 kg/m3 – 1010kg/m3, maximum dry density
(MDD) ranging from 670 kg/m3 – 890kg/m3 and optimum moisture content (OMC)
varying from 7.75 – 18.75% and classifying as A6/7 AASHTO materials. Other clay
minerals were identified and XRD analysis with mineralogical intensities range
from 10cts – >15cts showed CBR strength as high as 12.28% and classifying as
A-4 (silts) and A-2 AASHTO materials in stable highway sections.
Keywords: Clay minerals, Engineering
properties, composite and permeable pavement.