Monitoring and numerical modelling of riverbank erosion processes: a case study along the Cecina River (central Italy)
Monitoring and numerical modelling of riverbank erosion processes: a case study along the Cecina River (central Italy)
Riverbank retreat along a bend of the Cecina River, Tuscany (central Italy) was monitored across a near annual cycle (autumn 2003 to summer 2004) with the aim of better understanding the factors influencing bank changes and processes at a seasonal scale. Seven flow events occurred during the period of investigation, with the largest having an estimated return period of about 1·5 years. Bank simulations were performed by linking hydrodynamic, fluvial erosion, groundwater flow and bank stability models, for the seven flow events, which are representative of the typical range of hydrographs that normally occur during an annual cycle. The simulations allowed identification of (i) the time of onset and cessation of mass failure and fluvial erosion episodes, (ii) the contributions to total bank retreat made by specific fluvial erosion and mass-wasting processes, and (iii) the causes of retreat. The results show that the occurrence of bank erosion processes (fluvial erosion, slide failure, cantilever failure) and their relative dominance differ significantly for each event, depending on seasonal hydrological conditions and initial bank geometry. Due to the specific planimetric configuration of the study bend, which steers the core of high velocity fluid away from the bank at higher flow discharges, fluvial erosion tends to occur during particular phases of the hydrograph. As a result fluvial erosion is ineffective at higher peak discharges, and depends more on the duration of more moderate discharges. Slide failures appear to be closely related to the magnitude of peak river stages, typically occurring in close proximity to the peak phase (preferentially during the falling limb, but in some cases even before the peak), while cantilever failures more typically occur in the late phase of the flow hydrograph, when they may be induced by the cumulative effects of any fluvial erosion.
riverbank erosion, riverbank retreat, fluvial erosion, mass failures, cecina river, italy
530-546
Luppi, Laura
07c56f66-5e82-474c-b37b-65719cbeae7d
Rinaldi, Massimo
37a99621-c79d-4555-8d99-ea59c499c12f
Teruggi, Liliana B.
ed455ca1-d159-46a6-96ee-038e65afa791
Darby, Stephen E.
4c3e1c76-d404-4ff3-86f8-84e42fbb7970
Nardi, Laura
fe64639f-a04b-4894-9941-4786ea125404
2009
Luppi, Laura
07c56f66-5e82-474c-b37b-65719cbeae7d
Rinaldi, Massimo
37a99621-c79d-4555-8d99-ea59c499c12f
Teruggi, Liliana B.
ed455ca1-d159-46a6-96ee-038e65afa791
Darby, Stephen E.
4c3e1c76-d404-4ff3-86f8-84e42fbb7970
Nardi, Laura
fe64639f-a04b-4894-9941-4786ea125404
Luppi, Laura, Rinaldi, Massimo, Teruggi, Liliana B., Darby, Stephen E. and Nardi, Laura
(2009)
Monitoring and numerical modelling of riverbank erosion processes: a case study along the Cecina River (central Italy).
Earth Surface Processes and Landforms, 34, .
(doi:10.1002/esp.1754).
Abstract
Riverbank retreat along a bend of the Cecina River, Tuscany (central Italy) was monitored across a near annual cycle (autumn 2003 to summer 2004) with the aim of better understanding the factors influencing bank changes and processes at a seasonal scale. Seven flow events occurred during the period of investigation, with the largest having an estimated return period of about 1·5 years. Bank simulations were performed by linking hydrodynamic, fluvial erosion, groundwater flow and bank stability models, for the seven flow events, which are representative of the typical range of hydrographs that normally occur during an annual cycle. The simulations allowed identification of (i) the time of onset and cessation of mass failure and fluvial erosion episodes, (ii) the contributions to total bank retreat made by specific fluvial erosion and mass-wasting processes, and (iii) the causes of retreat. The results show that the occurrence of bank erosion processes (fluvial erosion, slide failure, cantilever failure) and their relative dominance differ significantly for each event, depending on seasonal hydrological conditions and initial bank geometry. Due to the specific planimetric configuration of the study bend, which steers the core of high velocity fluid away from the bank at higher flow discharges, fluvial erosion tends to occur during particular phases of the hydrograph. As a result fluvial erosion is ineffective at higher peak discharges, and depends more on the duration of more moderate discharges. Slide failures appear to be closely related to the magnitude of peak river stages, typically occurring in close proximity to the peak phase (preferentially during the falling limb, but in some cases even before the peak), while cantilever failures more typically occur in the late phase of the flow hydrograph, when they may be induced by the cumulative effects of any fluvial erosion.
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Published date: 2009
Keywords:
riverbank erosion, riverbank retreat, fluvial erosion, mass failures, cecina river, italy
Identifiers
Local EPrints ID: 65394
URI: http://eprints.soton.ac.uk/id/eprint/65394
ISSN: 0197-9337
PURE UUID: 8211de88-2f16-4a8b-ae9f-06c12de150a9
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Date deposited: 06 Feb 2009
Last modified: 14 Mar 2024 02:41
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Contributors
Author:
Laura Luppi
Author:
Massimo Rinaldi
Author:
Liliana B. Teruggi
Author:
Laura Nardi
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