Gravel-bed rivers display a surface layer that is coarser than the substrate lining below this armored surface. The armored layer that is developed under certain flow conditions may be attributed as water-worked sediment bed. Both the threshold of incipient motion and the bed-load transport are affected by the presence of this layer. In this study, the coarse surface development and its effect on the sediment transport were investigated experimentally in a rectangular flume. Four antecedent flow rates were combined with an input hydrograph, without sediment feeding. The reference shear stress of individual fractions and the grain-size distribution were determined after the development of the coarse surface due to the antecedent flow. Then a...
Mountain gravel-bed rivers typically display a surface layer that is armored. That is, the surface l...
A flume experiment was conducted to examine the evolution of a sand-gravel reach under a lack of sed...
Graduation date: 1973Presentation date: 1973-05-03Sediment transport in a gravel-bottomed stream loc...
Gravel-bed rivers display a surface layer that is coarser than the substrate lining below this armor...
Two sets of triangular hydrographs were generated in a 12-m-long laboratory flume for two sets of in...
Almost all sediment transport equations incorporate the Shields parameter, which is a ratio of the t...
Natural fluvial channels can experience significant variations in sediment transport rates under uns...
Explicit coupling between channel morphology and sediment transport requires a modeling approach in ...
One of the key problems in the research on fluvial hydraulics is to correctly reproduce the flow dyn...
In natural rivers, significant bedload transport and variability in sediment bed geomorphology is ge...
A laboratory study was undertaken to investigate how changes in flow regime and hydrograph shape (nu...
International audienceField measurements indicate that, in gravel bed rivers, bed load may not be a ...
Fluvial channels can experience significant variations to both sediment transport rates and deformat...
Differences in the structure of mobile armors formed at three different flow strengths have been inv...
Mountain gravel-bed rivers typically display a surface layer that is armored. That is, the surface l...
Mountain gravel-bed rivers typically display a surface layer that is armored. That is, the surface l...
A flume experiment was conducted to examine the evolution of a sand-gravel reach under a lack of sed...
Graduation date: 1973Presentation date: 1973-05-03Sediment transport in a gravel-bottomed stream loc...
Gravel-bed rivers display a surface layer that is coarser than the substrate lining below this armor...
Two sets of triangular hydrographs were generated in a 12-m-long laboratory flume for two sets of in...
Almost all sediment transport equations incorporate the Shields parameter, which is a ratio of the t...
Natural fluvial channels can experience significant variations in sediment transport rates under uns...
Explicit coupling between channel morphology and sediment transport requires a modeling approach in ...
One of the key problems in the research on fluvial hydraulics is to correctly reproduce the flow dyn...
In natural rivers, significant bedload transport and variability in sediment bed geomorphology is ge...
A laboratory study was undertaken to investigate how changes in flow regime and hydrograph shape (nu...
International audienceField measurements indicate that, in gravel bed rivers, bed load may not be a ...
Fluvial channels can experience significant variations to both sediment transport rates and deformat...
Differences in the structure of mobile armors formed at three different flow strengths have been inv...
Mountain gravel-bed rivers typically display a surface layer that is armored. That is, the surface l...
Mountain gravel-bed rivers typically display a surface layer that is armored. That is, the surface l...
A flume experiment was conducted to examine the evolution of a sand-gravel reach under a lack of sed...
Graduation date: 1973Presentation date: 1973-05-03Sediment transport in a gravel-bottomed stream loc...