Bed Waves Generated by Internal Waves in Alluvial Channelsby Bartele de Jong, Twente Univ, Netherlands,
Document Type: Proceeding Paper
Part of: Sediment Transport Modeling
Abstract: The flow in an alluvial channel is conceived as a stratified flow both with respect to the velocity- and density-distribution. In such flows internal waves may occur which influence the generation of bed elevations. This paper presents a theory that explains for low-Froude-number flows the initiation of dunes and ripples by these waves on a flat bed. The theory is demonstrated by comparing theoretical and experimental results for the case of bed-load transport. However, an extension to the case of suspended-load transport is straightforward.
Subject Headings: Internal waves | Water waves | Alluvial channels | Bed loads | Channel flow | Wave generation | Water supply systems | Water stratification
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