Abstract: The three-dimensional geometry of fluvial sandbodies may be very complicated. Factors influencing this complexity include th processes of fluvial scour and incision, both of which can promote local or widespread increases in sandbody thickness. Incision, as caused by downstream relative base-level fall, produces entrenched valleys that control the location of subsequent alluvial deposits. A simple model is presented that attempts to quantify the scale of this extrinsic incision and, in turn, highlights everal sedimentary implications ofbase-level fall. In contrast, scour is an intrinsic process common to all fluvial systems, and is promoted by constriction, curvature or confluences within the major channels. Existing empirical el ...
Fluvial bedrock incision is driven by the impact of moving bedload particles. Mechanistic, sediment‐...
This paper presents the results of an experimental study about the pattern of local scouring generat...
The effect of the flood recession time on the local scour depth at bed sills in gravel deposits is e...
Designers are often required to produce safe and economic structures in rivers with erodible beds, w...
This study deals with the development of deep scour holes in the river bed of the Dutch Rhine delta ...
River incision into bedrock is an important part of fluvial geomorphology because it controls landsc...
Obstacle marks are instream bedforms, typically composed of an upstream frontal scour hole and a dow...
Experimental results on local scour in long contractions for uniform and nonuniform sediments (grave...
grantor: University of TorontoErosion and deposition by flowing water commonly produce pat...
Local scour around bridge piers has been recognised as one of the major causes of bridge failure. Si...
The preserved deposits of fluvial meander belts typically take the form of patchworks of sand-prone ...
The rivers in the South-West of The Netherlands flow over an erosion-resistant bed, consisting of pe...
A flume experiment was conducted to investigate the effect of lateral constrictions on the initiatio...
physical models to predict erosion and deposition caused by currents in tidal inlet channels. A scal...
The periodic removal of sand from the interstitial spaces between cobbles is extremely important for...
Fluvial bedrock incision is driven by the impact of moving bedload particles. Mechanistic, sediment‐...
This paper presents the results of an experimental study about the pattern of local scouring generat...
The effect of the flood recession time on the local scour depth at bed sills in gravel deposits is e...
Designers are often required to produce safe and economic structures in rivers with erodible beds, w...
This study deals with the development of deep scour holes in the river bed of the Dutch Rhine delta ...
River incision into bedrock is an important part of fluvial geomorphology because it controls landsc...
Obstacle marks are instream bedforms, typically composed of an upstream frontal scour hole and a dow...
Experimental results on local scour in long contractions for uniform and nonuniform sediments (grave...
grantor: University of TorontoErosion and deposition by flowing water commonly produce pat...
Local scour around bridge piers has been recognised as one of the major causes of bridge failure. Si...
The preserved deposits of fluvial meander belts typically take the form of patchworks of sand-prone ...
The rivers in the South-West of The Netherlands flow over an erosion-resistant bed, consisting of pe...
A flume experiment was conducted to investigate the effect of lateral constrictions on the initiatio...
physical models to predict erosion and deposition caused by currents in tidal inlet channels. A scal...
The periodic removal of sand from the interstitial spaces between cobbles is extremely important for...
Fluvial bedrock incision is driven by the impact of moving bedload particles. Mechanistic, sediment‐...
This paper presents the results of an experimental study about the pattern of local scouring generat...
The effect of the flood recession time on the local scour depth at bed sills in gravel deposits is e...