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Showing papers by "Jørgen Fredsøe published in 1974"


Journal ArticleDOI
TL;DR: In this article, a two-dimensional stability analysis of the flow in a straight alluvial channel has been carried out, using the vorticity transport equation, and an attempt has been made to account for the influence of gravity on bed-load transport, and this turned out to change the stability quite significantly.
Abstract: A two-dimensional stability analysis of the flow in a straight alluvial channel has been carried out, using the vorticity transport equation. In the analysis an attempt has been made to account for the influence of gravity on bed-load transport, and this turned out to change the stability quite significantly.In the case of instability, the further growth of the dunes has been investigated using a second-order approximation, This nonlinear theory explains the experimental fact that the dunes very soon become asymmetric.

240 citations


Journal ArticleDOI
TL;DR: In this article, the shape of the irregularity is described using Fourier transforms, and the velocity profile in the unidirectional flow is determined using the eddy-viscosity concept and a finite wall slip velocity.
Abstract: Rotational flow of an inviscid fluid over an irregularity in the bottom is investigated. The flow is regarded as a perturbed unidirectional flow, and the shape of the irregularity is described using Fourier transforms. The velocity profile in the unidirectional flow is determined using the eddy-viscosity concept and a finite wall slip velocity. Two different examples of irregularities are considered: ( a ) an infinitely long straight irregularity which forms an arbitrary angle with the direction of the basic flow and ( b ) a hump in a channel with impermeable walls. The influence of rotation on the two- and three-dimensional waves which are formed downstream of these irregularities is analysed and experimentally verified. Further, it is shown that the gradient of the basic velocity profile increases the transverse movement of the fluid particles at the bottom, while at the surface this transverse movement is decreased.

9 citations