Skip to main content

Research Repository

Advanced Search

Bedform genesis in bedrock substrates: Insights into formative processes from a new experimental approach and the importance of suspension-dominated abrasion

Yin, Daowei; Peakall, Jeff; Parsons, Dan; Chen, Zhongyuan; Averill, Heather Macdonald; Wignall, Paul; Best, Jim

Authors

Daowei Yin

Jeff Peakall

Dan Parsons

Zhongyuan Chen

Heather Macdonald Averill

Paul Wignall

Jim Best



Abstract

© 2015 Elsevier B.V. Bedrock channels are common in the natural environment, and bedrock channel erosion sets the pace of denudation in many river catchments. However, in comparison to the large number of studies concerning the formation of alluvial bedforms, relatively few investigations have concerned bedrock bedform genesis. Field-based analysis of sculptured forms within bedrock channels has been restricted notably by the slow rate of bedform development in such environments. Furthermore, only a limited number of flume-scale experiments have been conducted that attempt to simulate the genesis of sculpted bedforms in bedrock channels. This study demonstrates that optimisation of clay beds through analysis of clay strength enables the development of features analogous to bedrock river channel bedforms - even at a scale that is orders of magnitude smaller than some natural examples. Three sets of suspended sediment-laden experiments were carried out using hard, medium, and soft clay bed substrates. A suite of erosive bedforms (including potholes, flutes, and furrows) developed on all experimental beds. All observed erosional features have clear equivalents to those observed in natural bedrock rivers. Bed shear strength was found to be a significant factor for the genesis of different types of simulated bedrock bedforms in our experiments with other factors, such as flow velocity, bed slope, and flow depth held approximately constant. Importantly, in a subset of experiments performed with an absence of suspended sediment, fluid flow did not result in the erosion and development of bedforms in the clay bed. Hence, this work illustrates that abrasion by suspended sediments is the key process required for the formation of these simulated bedrock bedforms in our experiments, in the absence of bedload abrasion; other processes such as plucking, cavitation, and dissolution will have been negligible.

Citation

Yin, D., Peakall, J., Parsons, D., Chen, Z., Averill, H. M., Wignall, P., & Best, J. (2016). Bedform genesis in bedrock substrates: Insights into formative processes from a new experimental approach and the importance of suspension-dominated abrasion. Geomorphology, 255, 26-38. https://doi.org/10.1016/j.geomorph.2015.12.008

Journal Article Type Article
Acceptance Date Dec 14, 2015
Online Publication Date Dec 17, 2015
Publication Date Feb 15, 2016
Deposit Date Dec 21, 2016
Publicly Available Date Dec 21, 2016
Journal Geomorphology
Print ISSN 0169-555X
Electronic ISSN 1872-695X
Publisher Elsevier
Peer Reviewed Not Peer Reviewed
Volume 255
Pages 26-38
DOI https://doi.org/10.1016/j.geomorph.2015.12.008
Keywords Physical modelling; Bedrock bedforms; Bedrock erosion; Suspension-dominated abrasion
Public URL https://hull-repository.worktribe.com/output/446429
Publisher URL http://www.sciencedirect.com/science/article/pii/S0169555X15302294
Additional Information Authors' accepted manuscript of article: Yin, J Peakall, D Parsons, Z Chen, HM Averill, P Wignall, J Best, Bedform genesis in bedrock substrates: Insights into formative processes from a new experimental approach and the importance of suspension-dominated abrasion, Geomorphology 255, 26-38

Files





You might also like



Downloadable Citations