Fluvial instabilities

Dey, Subhasish and Ali, S K Zeeshan (2020) Fluvial instabilities. American Institute of Physics Inc..

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Abstract

Fluvial instabilities originate from an interplay between the carrier fluid and the erodible loose boundary at their interface, manifesting a variety of sedimentary architectures with length scales spanning from a few millimeters to hundreds of meters. This review sheds light on the current state-of-the-science of the subject, explaining the fluvial instabilities from three broad perspectives. They are micro-scale, meso-scale, and macro-scale instabilities. The interactions between the near-bed hydrodynamics and the sediment dynamics in generating various kinds of instabilities, including their natures and driving mechanisms, are thoroughly appraised in the light of laboratory experimental results, field observations, and theoretical backgrounds. Besides, this review addresses the current challenges, delineating key points as a future research scope. © 2020 Author(s).

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IITH Creators:
IITH CreatorsORCiD
Ali, S K Zeeshanhttps://orcid.org/0000-0003-0763-7437
Item Type: Other
Uncontrolled Keywords: Carrier fluids; Driving mechanism; Field observations; Length scale; Macro scale; Meso scale; Sediment dynamic; Sedimentary architecture
Subjects: Civil Engineering
Divisions: Department of Civil Engineering
Depositing User: . LibTrainee 2021
Date Deposited: 23 Nov 2022 12:59
Last Modified: 23 Nov 2022 12:59
URI: http://raiithold.iith.ac.in/id/eprint/11170
Publisher URL: https://doi.org/10.1063/5.0010038
OA policy: https://v2.sherpa.ac.uk/id/publication/9872
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