Bed forms in channels result from the interaction between sediment transport, turbulence and gravitational settling. They document mechanisms of self-organization between flow structures and the developing structure of the bed. It is shown that these mechanisms can be characterized by length scales of the sediment, the bed form and the flow structure. Three types of interaction can be distinguished: 1) The first type of mechanisms can be observed at beds of sediment with grain diameter smaller than the typical structural dimension of turbulence. It is shown how with increasing hydraulic loading of the bed a hydraulically smooth surface develops structures, which turn from “orange peel” to stripe and arrowhead patterns and finally into ripples. This group of bed forms is limited to a grain diameter of in viscous units. In the regime of the stripe structures drag reduction occurs. 2) If grains or bed forms reach a height, which leads to separation, a completely different regime prevails, which is determined by the self-organization of separation zones. A prominent example for these bed forms are dunes. 3) Demixing processes, secondary flows and roughness contrasts finally lead to the development of longitudinal and transverse banks. All three mechanisms are explained on the basis of kinematic models and documented by experimental data. Emphasis is put on the two-dimensionalization of bed forms in a highly 3-dimensional (3D) turbulent flow, which is traced back to the self organization of vortex systems. This review article contains 55 references.
Skip Nav Destination
Article navigation
January 2004
Review Articles
Bed forms in turbulent channel flow
Albert Gyr and,
Albert Gyr and
Institute of Hydromechanics and Water Resources Management, Swiss Federal Institute of Technology, Zurich, Switzerland; gyr@ihw.baug.ethz.ch
Search for other works by this author on:
Wolfgang Kinzelbach
Wolfgang Kinzelbach
Institute of Hydromechanics and Water Resources Management, Swiss Federal Institute of Technology, Zurich, Switzerland; gyr@ihw.baug.ethz.ch
Search for other works by this author on:
Albert Gyr and
Institute of Hydromechanics and Water Resources Management, Swiss Federal Institute of Technology, Zurich, Switzerland; gyr@ihw.baug.ethz.ch
Wolfgang Kinzelbach
Institute of Hydromechanics and Water Resources Management, Swiss Federal Institute of Technology, Zurich, Switzerland; gyr@ihw.baug.ethz.ch
Appl. Mech. Rev. Jan 2004, 57(1): 77-93 (17 pages)
Published Online: February 10, 2004
Article history
Online:
February 10, 2004
Citation
Gyr and , A., and Kinzelbach , W. (February 10, 2004). "Bed forms in turbulent channel flow ." ASME. Appl. Mech. Rev. January 2004; 57(1): 77–93. https://doi.org/10.1115/1.1584063
Download citation file:
Get Email Alerts
Cited By
Fractal and Hurst effects in stochastic mechanics
Appl. Mech. Rev
Magnetohydrodynamics in liquid metal interfacial flows
Appl. Mech. Rev
Related Articles
Turbulence Structure Modification and Drag Reduction by Microbubble Injections in a Boundary Layer Channel Flow
J. Fluids Eng (November,2008)
PIV-POD Investigation of the Wake of a Sharp-Edged Flat Bluff Body Immersed in a Shallow Channel Flow
J. Fluids Eng (February,2009)
Investigation on Flow Field Characteristics by Drag Reducing Agent Additives in a Stirred Vessel
J. Energy Resour. Technol (October,2020)
Vortex Motion in a Swirling Flow of Surfactant Solution with Drag Reduction
J. Fluids Eng (January,2006)
Related Proceedings Papers
Related Chapters
Multiphase Flow Simulations of Sediment Particles in Mixed-flow Pumps
Mixed-flow Pumps: Modeling, Simulation, and Measurements
Cavitating Structures at Inception in Turbulent Shear Flow
Proceedings of the 10th International Symposium on Cavitation (CAV2018)
The Fog Sedimentation Rate Control and Simulation of Salt Spray System
International Conference on Information Technology and Computer Science, 3rd (ITCS 2011)