nerc.ac.uk

Morphodynamics and sedimentary structures of bedforms under supercritical-flow conditions: New insights from flume experiments

Cartigny, Matthieu J.B.; Ventra, Dario; Postma, George; van Den Berg, Jan H.; Venditti, Jeremy. 2014 Morphodynamics and sedimentary structures of bedforms under supercritical-flow conditions: New insights from flume experiments. Sedimentology, 61 (3). 712-748. 10.1111/sed.12076

Before downloading, please read NORA policies.
[thumbnail of CartignyRevisedManuscriptJuly2013.pdf]
Preview
Text
CartignyRevisedManuscriptJuly2013.pdf - Accepted Version

Download (327kB) | Preview

Abstract/Summary

in the stratigraphic record. This fact is commonly ascribed to the poor preservation potential of deposits from high-energy supercritical flows. However, the number of flume data sets on supercritical-flow dynamics and sedimentary structures is very limited in comparison with available data for subcritical flows, which hampers the recognition and interpretation of such deposits. The results of systematic flume experiments spanning a broad range of supercritical-flow bedforms (antidunes, chutes-and-pools and cyclic steps) developed in mobile sand beds of variable grain sizes are presented. Flow character and related bedform patterns are constrained through time-series measurements of bed configurations, flow depths, flow velocities and Froude numbers. The results allow the refinement and extension of some widely used bedform stability diagrams in the supercritical-flow domain, clarifying in particular the morphodynamic relations between antidunes and cyclic steps. The onset of antidunes is controlled by flows exceeding a threshold Froude number. The transition from antidunes to cyclic steps in fine to medium-grained sand occurs at a threshold mobility parameter. Sedimentary structures associated with supercritical bedforms developed under variable aggradation rates are revealed by means of combining flume results and synthetic stratigraphy. The sedimentary structures are compared with examples from field and other flume studies. Aggradation rate is seen to exert an important control on the geometry of supercritical-flow structures and should be considered when identifying supercritical bedforms in the sedimentary record.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1111/sed.12076
ISSN: 00370746
Additional Keywords: Antidunes; chutes-and-pools; cyclic steps; flume experiments; hydraulic jump; supercritical flow
Date made live: 06 Mar 2014 16:49 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/505415

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...