The Formation of Meandering and Braided Channelsby Gerd Holtorff, Technical Univ Berlin, Germany,
Document Type: Proceeding Paper
Part of: Sediment Transport Modeling
Flow in alluvial channels implies flow past boundaries that form and deform under the action of the flow. Interaction between the flow and the mobile boundaries produces channel patterns which are classified as meandering and braided. The present study shows that the amount of fine sediment contained in the bank-material which is suspended during the evolutionary process of the channel has an important bearing on whether the channel will develop into a meandering or braided channel.
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