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This study aims at reporÜng textural changes linked "vith real grain size trend evolutions seen on sands in coastal environnement. The oruy practical way consist in simulating removals or arrivaIs of particules, called movable populations, according to a law of deterrnined frequency. From t.'le formalized experimental distribution (first step) and the distribution of a movable population thus defined (second step), the consequent distribution is determined to reach a repartition coinciding, as precisely as possible, with the experimental distribution observed (down drift sediment or post-storm sediment). Severa! experiences have been realized frOIDsamples recovered in actual situations in the case of macrotidal sandy beaches, such as Merlimont in the Pasde-Calais or Omaha Beach in the Normandy. The results are presented and discussed. Granulométrie/ population mobile/ modélisation/ simulation

Mobilité sédimentaire : définition par simulation des populations granulométriques mobiles sur l'avant-côte