Advance, Retreat, and Halt of Abrupt Gravel-Sand Transitions in Alluvial Rivers

Blom, Astrid; Chavarrías, Víctor; Ferguson, Robert I.; Viparelli, Enrica

Abstract

Downstream fining of bed sediment in alluvial rivers is usually gradual, but often an abrupt decrease in characteristic grain size occurs from about 10 to 1 mm, i.e., a gravel-sand transition (GST) or gravel front. Here we present an analytical model of GST migration that explicitly accounts for gravel and sand transport and deposition in the gravel reach, sea level change, subsidence, and delta progradation. The model shows that even a limited gravel supply to a sand bed reach induces progradation of a gravel wedge and predicts the circumstances required for the gravel front to advance, retreat, and halt. Predicted modern GST migration rates agree well with measured data at Allt Dubhaig and the Fraser River, and the model qualitatively captures the behavior of other documented gravel fronts. The analysis shows that sea level change, subsidence, and delta progradation have a significant impact on the GST position in lowland rivers.

Citation

Blom, A., Chavarrías, V., Ferguson, R. I., & Viparelli, E. (2017). Advance, Retreat, and Halt of Abrupt Gravel-Sand Transitions in Alluvial Rivers. Geophysical Research Letters, 44(19), 9751-9760. https://doi.org/10.1002/2017gl074231

• Journal Article Type: Article
• Acceptance Date: Aug 25, 2016
• Online Publication Date: Oct 27, 2017
• Publication Date: 2017-10
• Deposit Date: Aug 15, 2019
• Journal: Geophysical Research Letters
• Print ISSN: 0094-8276
• Publisher: Wiley
• Peer Reviewed: Peer Reviewed
• Volume: 44
• Issue: 19
• Pages: 9751-9760
• DOI: https://doi.org/10.1002/2017gl074231
• Public URL: https://durham-repository.worktribe.com/output/1290418