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Bed-load transport for steady flows and unsteady oscillatory flows

Jan S. Ribberink
- 01 Jul 1998 - 
- Vol. 34, Iss: 34, pp 59-82
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TLDR
In this paper, the validity of a bed-load transport formula based on the bed-shear concept of Meyer-Peter and Mueller was investigated for steady unidirectional flows, oscillatory flows and oscillatory flow with superimposed net currents.
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This article is published in Coastal Engineering.The article was published on 1998-07-01. It has received 362 citations till now. The article focuses on the topics: Shields parameter.

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Citations
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Unified view of sediment transport by currents and waves. I: Initiation of motion, bed roughness, and bed-load transport

TL;DR: In this paper, the effect of fine silt on the bed composition and on initiation of motion (critical conditions) of sediment beds over the full range of conditions (silts to gravel) is discussed.
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The predictability of cross-shore bed evolution of sandy beaches at the time scale of storms and seasons using process-based Profile models

TL;DR: In this paper, the authors present information of coastal processes on these time scales and assess the predictive capabilities of Profile models with respect to hydrodynamics and morphodynamics at sandy beaches on the time scales of storms and seasons.
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On two-phase sediment transport: sheet flow of massive particles

TL;DR: In this paper, a model for concentrated sediment transport that is driven by strong, fully developed turbulent shear flows over a mobile bed is presented, where balance equations for the average mass, momentum and energy for the two phases are phrased in terms of concentration-weighted (Favre averaged) velocities.
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Review of wave‐driven sediment resuspension and transport in estuaries

TL;DR: A review of wave-driven sediment resuspension and transport in estuaries, including generation of bed shear stress by waves, initiation of sediment motion by waves and the ways waves modulate, add to, and interact with sediment transport driven by currents, can be found in this paper.
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Modeling cross-shore sandbar behavior on the timescale of weeks

TL;DR: In this paper, the authors compare predictions of a coupled, wave-averaged, cross-shore waves-currents-bathymetric evolution model to observations of onshore and offshore nearshore sandbar migration.
References
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Formulas for Bed-Load transport

E. Meyer-Peter, +1 more
TL;DR: In this article, an attempt is made to derive an empirical law of bed-load transport based on recent experimental data and the results and interpretation of tests already made known in former publications of the Laboratory for Hydraulic Research and Soil Mechanics at the Federal Institute of Technology, Zurich.

The Bed-Load Function for Sediment Transportation in Open Channel Flows

Abstract: CONTENTS Page Introduction. 1 Approach to the problem. _ 3 Limitation of the bed-load function _ _ _ 4 The undetermined function 4 The alluvial stream. 5 The sediment mixture 6 Hydraulics of the alluvial channel. 7 The friction formula 7 The friction factor 8 Resistance of the bars 9 The laminar sublayer 10 The transition between hydraulically rough and smooth beds_ 12 The velocity fluctuations 13 Suspension 14 The transportation rate of suspended load 17 Integration of the suspended load. _ 17 Numerical integration of suspended load 19 Limit of suspension. 24 The bed layer 24 Practical calculation of suspended load___ ____ 25 Numerical example 26 Page Bed-load concept 29 Some constants entering the laws of bed-load motion: 31 The bed-load equation 32 The exchange time 33 The exchange probability 34 Determination of the probability V 35 Transition between bed load and. suspended load 38 The necessary graphs 40 Flume tests with sediment mixtures.. 42 Sample calculation of a river reachl 44 Choice of a river reach 45 Description of a river reach_____ 45 Application of procedure to Big Sand Creek, Miss 46 Discussion of calculations 60 Limitations of the method____ 65 Summary. 67 Literature cited 68 Appendix 69 List of symbols. 69 Work charts _ 71
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A monograph on sediment transport in alluvial streams

TL;DR: In this article, the authors proposed the principle of similarity for the prediction of stage-discharge relations in alluvial streams. But they did not consider the effect of the number of particles in the stream.
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The flow of cohesionless grains in fluids

TL;DR: In this article, it was shown that if the bed is composed entirely of potentially mobile grains a stress-equilibrium relation at the bed surface can be defined whereby the magnitude of a certain "bed load" of grains in transit over unit bed area is given in terms of the applied tangential stress.