Evolution granulométrique des sols sablo-argileux soumis à des compactages dynamique et statique

The compaction of a quartz sand by the modified Proctor test involves the production of fines produced by the breaking of the grains of the sand. This production of fines is measured by the grain size analysis before and after compaction. The adding of clay to the sand diminishes the evolution of the grain size. The process is proportional to the quantity of clay added to the sand. If the dynamic compaction of the Proctor test is substituted by the static compaction, one notes the same occurrences: static or dynamic compaction breaks the grains of sand and the clay added to the sand protects the grains from the breaking induced by the compaction stresses.