Difference between revisions of "File:BlondeauxFig10.jpg"
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Dronkers J (talk | contribs) (The yellow sediment grains are coarser that the red sediments and pile up at the crests of the ripples which are generated in a U-tube by an oscillatory flow. The figure shows a top view of the bottom at two different phases of the cycle (adapted from...) |
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Latest revision as of 14:32, 5 June 2017
The yellow sediment grains are coarser that the red sediments and pile up at the crests of the ripples which are generated in a U-tube by an oscillatory flow. The figure shows a top view of the bottom at two different phases of the cycle (adapted from Foti E. and Blondeaux P. (1995). Sea ripple formation: the heterogeneous sediment case. Coastal Eng., 25(3-4), 237-253)
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| current | 14:32, 5 June 2017 |  | 1,451 × 578 (121 KB) | Dronkers J (talk | contribs) | The yellow sediment grains are coarser that the red sediments and pile up at the crests of the ripples which are generated in a U-tube by an oscillatory flow. The figure shows a top view of the bottom at two different phases of the cycle (adapted from... |
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