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Dans ce travail, nous nous sommes interesses a l'etat de surconsolidation d'un sediment marin provenant de la pente continentale du golfe de Guinee. Une attention particuliere a ete portee aux phenomenes physico-chimiques. L'etude s'est effectuee, d'une part, au niveau microscopique, en se basant sur la theorie de la double couche diffuse [6, 8, 12] et, d'autre part, au niveau macroscopique, a l'aide...
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