Measurements of suspended load carried by the Meuse river have been made during floods at eight locations distributed on the Belgian course of the river. Regression lines were obtained for the relationships between discharge of water and the amount of suspended load. Comparisons between the regressions at the different places indicate parts of the river where some sedimentation occurs and other parts where some new sediments are added in the river bed.

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Measurements of suspended load carried by the Meuse river have been made during floods at eight locations distributed on the Belgian course of the river. Regression lines were obtained for the relationships between discharge of water and the amount of suspended load. Comparisons between the regressions at the different places indicate parts of the river where some sedimentation occurs and other parts where some new sediments are added in the river bed.

Marc VROLIX & Albert PISSART: Étude des variations de la charge en suspension de la Meuse entre Hastiere et Lixhe; 25 (1990/1) - Rivières : formes, processus, milieu de vie

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