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An approach to the sediment transport problem from general physics

R. A. Bagnold
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The article was published on 1966-01-01 and is currently open access. It has received 1796 citations till now. The article focuses on the topics: Sediment transport & Rouse number.

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Citations
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Sediment transport; Part I, Bed load transport

TL;DR: In this article, a method is presented which enables the computation of the bed-load transport as the product of the saltation height, the particle velocity and the bed load concentration.
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Development and validation of a three-dimensional morphological model

TL;DR: The DELFT3D-FLOW module as discussed by the authors is a 3D flow solver for modeling sediment transport patterns in the water column of the DELFT-3D flow model, which is used to model both suspended and bedload transport of noncohesive sediment.
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Sediment Transport, Part II: Suspended Load Transport

TL;DR: In this article, a method is presented which enables the computation of the suspended load as the depth-integration of the product of the local concentration and flow velocity, based on the calculation of the reference concentration from the bed-load transport.
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A genetic classification of floodplains

TL;DR: In this paper, the relation between a stream's ability to entrain and transport sediment and the erosional resistance of floodplain alluvium that forms the channel boundary provides the basis for a genetic classification of floodplains.
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Turbidity Currents Generated at River Mouths during Exceptional Discharges to the World Oceans

TL;DR: In this article, a marine hyperpycnal plume is a particular kind of turbidity current occurring at a river mouth when the concentration of suspended sediment is so large that the density of the river water is greater than the densities of sea water.
References
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Equilibrium‐conditions in debris‐laden streams

TL;DR: Gilbert as mentioned in this paper formulated the major principles of stream-work and land-sculpture in a paper (G. K. Gilbert, Report on the geology of the Henry Mountains, U.S. Geog. and Geol. Sur. of the Rocky Mountain Region, pp. 99-150, 1877).
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Energy-balance in stream-flows carrying suspended load

TL;DR: In this paper, a general expression of stream-equilibrium in the form of an energy-equation is proposed, where the loss in potential energy of the flowing mixture plus the decrease in kinetic energy of flow is equated to the energy consumed in friction plus the energy consumption in supporting the debris.