Geography Publications

Document Type

Article

Publication Date

9-19-2018

Volume

44

Issue

1

Journal

Earth Surface Processes and Landforms

First Page

304

Last Page

316

URL with Digital Object Identifier

https://doi.org/10.1002/esp.4511

Abstract

Evolution of bed material mobility and bedload grain size distributions under a range of discharges is rarely observed in braiding in gravel-bed rivers. Yet, the changing of bedload grain size distributions with discharge is expected to be different from laterally stable, threshold, channels on which most gravel bedload theory and observation are based. Here, simultaneous observations of flow, bedload transport rate, and morphological change were made in a physical model of a gravel-bed braided river to document the evolution of grain size distributions and bed mobility over three experimental event hydrographs. Bedload transport rate and grain size distributions were measured from bedload samples collected in sediment baskets. Morphological change was mapped with high-resolution (~1 mm precision) digital elevation models generated from close-range digital photogrammetry. Bedload transport rates were extremely low below a discharge equivalent to ~50 % of the channel-forming discharge (dimensionless stream power ~70). Fractional transport rates and plots of grain size distributions indicate that the bed experienced partial mobility at low discharge when the coarsest grains on the bed were immobile, weak selective mobility at higher discharge, and occasionally near-equal mobility at peak channel-forming discharge. The transition to selective mobility and increased bedload transport rates coincided with the lower threshold for morphological change measured by the morphological active depth and active width. Below this threshold discharge, active depths were of the order of D90 and active widths narrow (< 3% of wetted width). Above this discharge, both increased so that at channel forming discharge, the active depth had a local maximum of 9D90 while active width was up to 20% of wetted width. The modelled rivers approached equal mobility when rates of morphological change were greatest. Therefore, changes 38 in the morphological active layer with discharge is directly connected to the conditions bed mobility, and strongly correlated with bedload transport rate.

Notes

This is the peer reviewed version of the following article: Peirce, S., Ashmore, P. & Leduc, P. (2019) Evolution of grain size distributions and bed mobility during mydrographs in gravel-bed braided rivers. Earth Surface Processes and Landforms 44(1), 304-316, which has been published in final form at https://doi.org/10.1002/esp.4511 . This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions.

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