Back-flow ripples in troughs downstream of unit bars: Formation, preservation and value for interpreting flow conditions

Herbert, Christopher, Alexander, Jan ORCID: https://orcid.org/0000-0002-2830-2727 and Martinez De Alvaro, Maria (2015) Back-flow ripples in troughs downstream of unit bars: Formation, preservation and value for interpreting flow conditions. Sedimentology, 62 (7). 1814–1836. ISSN 0037-0746

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Abstract

Back-flow ripples are bedforms created within the lee-side eddy of a larger bedform with migration directions opposed or oblique to that of the host bedform. In the flume experiments described in this article, back-flow ripples formed in the trough downstream of a unit bar and changed with mean flow velocity; varying from small incipient back-flow ripples at low velocities, to well-formed back-flow ripples with greater velocity, to rapidly migrating transient back-flow ripples formed at the greatest velocities tested. In these experiments back-flow ripples formed at much lower mean back-flow velocities than predicted from previously published descriptions. This lower threshold mean back-flow velocity is attributed to the pattern of velocity variation within the lee-side eddy of the host bedform. The back-flow velocity variations are attributed to vortex shedding from the separation zone, wake flapping and increases in the size of, and turbulent intensity within, the flow separation eddy controlled by the passage of superimposed bedforms approaching the crest of the bar. Short duration high velocity packets, whatever their cause, may form back-flow ripples if they exceed the minimum bed shear stress for ripple generation for long enough or, if much faster, may wash them out. Variation in back-flow ripple cross-lamination has been observed in the rock record and, by comparison with flume observations, the preserved back-flow ripple morphology may be useful for interpreting formative flow and sediment transport dynamics.

Item Type: Article
Additional Information: © 2015 The Authors. Sedimentology published by John Wiley & Sons Ltd on behalf of International Association of Sedimentologists. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
Uncontrolled Keywords: back-flow ripples,bedforms,bottomsets,counter-current ripples,ripples,ripple cross-lamination
Faculty \ School: Faculty of Science
Faculty of Science > School of Environmental Sciences
UEA Research Groups: Faculty of Science > Research Groups > Geosciences
Faculty of Science > Research Groups > Geosciences and Natural Hazards (former - to 2017)
Depositing User: Pure Connector
Date Deposited: 24 Jul 2015 22:57
Last Modified: 21 Oct 2022 01:01
URI: https://ueaeprints.uea.ac.uk/id/eprint/53767
DOI: 10.1111/sed.12203

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