
The aim of this study was to identify, classify and characterize the activities and correlations between the intrinsic properties of the four lateritic gravels used in construction. The grading curves of the four lateritic gravelly are spread out, but poorly calibrated. Lateritic gravel LG1 contains class B5 silty fines with low plasticity and low swelling. Lateritic gravels LG2, LG3 and LG4 contain clayey fines of low plasticity and medium swelling, class B6. The specific surface area and cation exchange capacity depend on the mineralogy, organic composition and texture of the lateritic gravel. The blue value of the soil characterizes the activity of the clay fines and reflects the surface activity of the lateritic gravels. The four lateritic gravels are inactive and contain minerals (kaolinite, quartz, goethite, hematite). The correlations obtained between the intrinsic properties are linear fits and between the liquidity limit and the specific surface area a non-linear fit of the ExpDec1 model with R2 (0.99). The relationship between activity and surface activity is simply the relative activity.
Atterberg Limit, Mineralogy, CBR, Activity, Specific Surface Area, Cation Exchange Capacity
Atterberg Limit, Mineralogy, CBR, Activity, Specific Surface Area, Cation Exchange Capacity
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