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dc.rights.licenseCC-BY-NC-ND
dc.contributor.advisorPostma, G.
dc.contributor.authorPoos, W.J.R.
dc.date.accessioned2011-12-15T18:01:18Z
dc.date.available2011-12-15
dc.date.available2011-12-15T18:01:18Z
dc.date.issued2011
dc.identifier.urihttps://studenttheses.uu.nl/handle/20.500.12932/9746
dc.description.abstractWater flowing over a bed made of silici-clastic material forms bedforms. A stability diagram for these bedforms is available for the lower flow regime where the Froude number < 0.8. No such diagram is available for the upper flow regime (Fr > 0.8). Experiments in a tiltable flume show that the bedforms for the upper flow regime can be characterized as: upper plane bed, antidunes, chute and pools and cyclic steps. These bedforms are plotted in a stability showing the relation between the dimensionless grain size and the ratio of minimum and maximum Froude number (before and after the hydraulic jump if present) showing proof of concept for such a stability diagram.
dc.description.sponsorshipUtrecht University
dc.format.extent1220414 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleStability Diagram of upper flow regime bedforms. An experimental study
dc.type.contentMaster Thesis
dc.rights.accessrightsOpen Access
dc.subject.keywordsupper, flow, regime, supercritical, cyclic, step, antidunes, chute, pools, experimental
dc.subject.courseuuGeology


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