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Earth Surface Dynamics An interactive open-access journal of the European Geosciences Union
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Discussion papers
https://doi.org/10.5194/esurf-2017-7
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esurf-2017-7
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Submitted as: research article 14 Feb 2017

Submitted as: research article | 14 Feb 2017

Review status
This discussion paper is a preprint. It has been under review for the journal Earth Surface Dynamics (ESurf). A final paper in ESurf is not foreseen.

Long-term Morphodynamics of a Schematic River Analysed with a Zero-dimensional, Two-reach, Two-grainsize Model

Mariateresa Franzoia1, Michael Nones2, and Giampaolo Di Silvio1 Mariateresa Franzoia et al.
  • 1Department of Civil, Architectural and Environmental Engineering, University of Padua, via Loredan 20, 35100, Italy
  • 2Interdepartmental Centre for Industrial Research in Building and Construction – Fluid Dynamics Unit, University of Bologna, Italy, via del Lazzaretto 15/5, 40121 Bologna, Italy

Abstract. At the basin scale, neglecting localized deviations caused by geological constraints like knick-points, alluvial rivers commonly exhibit a concave profile and a progressive sediment fining in the downstream direction. Although this configuration is, perforce, not in equilibrium, yet it usually shows a quasi-stationary behaviour at the very long (historical and geological) time-scale.

A zero-dimensional, two-reach, two-grainsize hydro-morphological model is presented and applied to a schematic river. The description of the processes involved is done assuming several reasonable and verified simplifications, giving reason of the extremely slow evolution of many alluvial rivers and providing a quantitative approach to evaluate their response time. Different from previous analytical formulations, the response time appears here to be affected, among others, by the granulometry of the sediment input.

Applications of the model to different geometries demonstrate that the present riverine morphology at the basin scale will persist practically stationary for extremely long periods of time (centuries and even millennia), if the climatic forcing remain unchanged and no anthropogenic perturbations are introduced in the system.

Mariateresa Franzoia et al.
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Interactive discussion
Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Mariateresa Franzoia et al.
Mariateresa Franzoia et al.
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Short summary
Describing the long-term evolution of rivers can be very challenging, especially because of the computational effort required by a detailed description of the physical processes involved. To address this problem, simplified physically-based models can represent an innovative approach, but a thorough verification of equations and simplifications adopted is strictly required. In this work, a 0D, two-reach, two-grainsize hydro-morphological model is presented and applied to a schematic reach.
Describing the long-term evolution of rivers can be very challenging, especially because of the...
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