Abstract
Shallow water equations (SWEs) have been traditionally derived by integrating fundamental flow equations over a flow profile above a single point in a horizontal or nearly horizontal plane, with the main assumptions that the profile thickness is much smaller than other two dimensions and it contains only water. This paper presents the derivation of generalized SWEs (GSWEs) obtained for a finite plan area, allowing for the presence of phases other than water, such as air, grains, vegetation, and debris, which can be either stationary or mobile. The derivation provides a rigorous basis for various applications of layer-averaged models and opens numerous research questions, some of which are highlighted in the paper.
Original language | English |
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Pages (from-to) | 303-321 |
Number of pages | 19 |
Journal | Journal of Hydraulic Research |
Volume | 61 |
Issue number | 3 |
Early online date | 26 Jul 2023 |
DOIs | |
Publication status | Published - 26 Jul 2023 |
Bibliographical note
AcknowledgmentsThe author would like to thank Vladimir Nikora and Mohamed Ghidaoui for the invitation to write this Vision Paper. Rui Ferreira and Francesco Ballio have provided thorough reviews of the initial draft. Their time and effort, thoughtful comments, and helpful suggestions are gratefully acknowledged.
The application of the double-averaging methodology to open channel flows had been developed and discussed with an informal group of researchers, who held eight workshops in the period between 2002 and 2010. The author would like to thank Vladimir Nikora for the leadership of this group and all group members for many enjoyable, challenging and productive discussions.
Funding
The author is grateful to the UK's Engineering and Physical Sciences Research Council (EPSRC, grants GR/R51865/01, EP/E0113301, and EP/K013513/1) and School of Engineering at the University of Aberdeen for the funding support towards this work.
Keywords
- Aerated flows
- bed-load
- debris-flows
- rough bed
- SWEs
- vegetated channels