The influence of mineralogical compositions on geotechnical properties of two
genetically different soils around the northern part of Ondo State, Nigeria, was
evaluated to better understand the complex engineering performance of clayey soils
as derived by the parent rock. The soil samples collected from the region were
subjected to XRD analysis, index strength tests, and statistical analysis. Geological
mapping revealed Charnockite (Ch) and medium- to coarse-grained granite (OGe)
rock types in the area. The OGe-derived soils have a dominance of low-activity clay
mineral 1:1. On the other hand, the Ch-derived soils have a dominance of highactivity
clay minerals of 2:1. The statistical analysis showed that there is no significant
soil variation based on the size of its particle; however, it indicates that there is a
significant difference in the coefficient of variations of their respective moisture
content. Furthermore, Ch and OGe CBR values indicate a significant difference of 86
coefficients of variation, which account for a 75.61% reduction in the strength values
between the two soil types. Ch-derived soil samples plot within the CH region of the
plasticity chart, while OGe-derived soil samples plot within the CI region. Chderived
and OGe-derived soils have optimum moisture content (OMC) mean values
that fall above and within FMWH, (1997) recommended specifications, respectively.
Ch-derived soils have a lower bearing capacity compared to OGe-derived soils. The
OGe-derived soils have different and preferred engineering properties compared to
the Ch-derived soils due to mineralogical differences. Hence, mineralogical
characteristics of the parent material are responsible for behavioral differences in the
engineering properties of soils derived from genetically different parent rock.
Keywords: Clay minerals, Geotechnical properties, Engineering soils, Statistical
analysis.
