Treatise on Geomorphology 2013
DOI: 10.1016/b978-0-12-374739-6.00233-5
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9.8 Bedload Kinematics and Fluxes

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Cited by 28 publications
(4 citation statements)
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References 204 publications
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“…Unlike water and sediment dynamics, for which extensive research commenced at the beginning of the twentieth century [ Haschenburger , ], research on large wood dynamics in rivers has only become an important focus for research over the last three decades. As a result, this research remains at a relatively early stage, perhaps similar to that reached in the 1960s for water or suspended sediment monitoring, with many fundamental questions still open.…”
Section: Remaining Challengesmentioning
confidence: 99%
“…Unlike water and sediment dynamics, for which extensive research commenced at the beginning of the twentieth century [ Haschenburger , ], research on large wood dynamics in rivers has only become an important focus for research over the last three decades. As a result, this research remains at a relatively early stage, perhaps similar to that reached in the 1960s for water or suspended sediment monitoring, with many fundamental questions still open.…”
Section: Remaining Challengesmentioning
confidence: 99%
“…In gravel‐bed alluvial rivers, episodic bed material transport is the most significant factor controlling a river evolution and morphodynamic processes (Ashmore, ; Church, ; Church & Ferguson, ; Ferguson, ). A reliable estimation of bed material transport is a key issue to address several questions (e.g., river morphodynamics study and flood risk management), but it is notoriously hard to achieve (Ferguson, ; Haschenburger, ). One of the most used solutions to address this issue is through theoretically based formulas (e.g., Recking et al, ), but often the application of different relations proposed for a given context provides strongly incongruent estimates (Gomez & Church, ; López et al, ; Martin & Ham, ).…”
Section: Introductionmentioning
confidence: 99%
“…Washload requires so little energy to be transported that it tends to remain in suspension for hours or days even in areas of still water. Bedload transport is typically discontinuous in time and space (Haschenburger, 2013). Figure 8 Simplified illustration of hydraulics in a natural channel.…”
Section: Sediment Transport In Streamsmentioning
confidence: 99%