Formation of stationary alternate bars i
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Thomas E. Lisle; Hiroshi Ikeda; Fujiko Iseya
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Article
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1991
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John Wiley and Sons
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English
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Alternate bars were formed by sediment transport in a flume with Froude-modelled flow and relative roughness characteristic of gravel-boulder channels with steep slopes. The flume (0.3 m wide x 7.5 m long) was filled with a sand-gravel mixture, which was also fed into the top of the flume at a const