Modelling badlands erosion with SHETRAN at Draix, southeast France
Modelling badlands erosion with SHETRAN at Draix, southeast France
The physically-based, distributed flow and sediment transport modelling system SHETRAN was applied to the Draix basins to test its ability to represent badlands flow and erosion response, to quantify characteristic parameter values and to investigate spatial scale effects in badlands modelling. A unit gully, area 0.133 ha, was simulated using a 5-m grid resolution model and a single cell model, with comparable results. Application of the models to a badlands basin, area 86 ha, suggests that transfer of parameter sets from the gully scale to a larger scale may be feasible but, given uncertainty in parameter evaluation, a separate calibration still yields improved results. Considering the flashy basin responses, satisfactory flow simulations were achieved using physically realistic parameter values, and sediment yields were well simulated within the bounds of uncertainty. Any scale effects which may distinguish the gully and basin simulations are masked by the uncertainty in parameter evaluation.
129-136
Bathurst, James C.
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Lukey, Ben
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Sheffield, Justin
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Hiley, Robert A.
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Mathys, Nicolle
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1998
Bathurst, James C.
aadaf6f2-aa08-41bf-94d3-b30321da34e3
Lukey, Ben
fcbb46e1-ba8c-42a7-800b-6605392373c6
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Hiley, Robert A.
6fb25937-9a80-44b8-854e-cc1f3ba2dcee
Mathys, Nicolle
4c5ef60e-2843-41b8-8b50-4b2f81bcba1e
Bathurst, James C., Lukey, Ben, Sheffield, Justin, Hiley, Robert A. and Mathys, Nicolle
(1998)
Modelling badlands erosion with SHETRAN at Draix, southeast France.
In Modelling Soil Erosion, Sediment Transport and Closely Related Hydrological Processe: Proceedings of a symposium held at Vienna, July 1998.
vol. 249,
IAHS Press.
.
Record type:
Conference or Workshop Item
(Paper)
Abstract
The physically-based, distributed flow and sediment transport modelling system SHETRAN was applied to the Draix basins to test its ability to represent badlands flow and erosion response, to quantify characteristic parameter values and to investigate spatial scale effects in badlands modelling. A unit gully, area 0.133 ha, was simulated using a 5-m grid resolution model and a single cell model, with comparable results. Application of the models to a badlands basin, area 86 ha, suggests that transfer of parameter sets from the gully scale to a larger scale may be feasible but, given uncertainty in parameter evaluation, a separate calibration still yields improved results. Considering the flashy basin responses, satisfactory flow simulations were achieved using physically realistic parameter values, and sediment yields were well simulated within the bounds of uncertainty. Any scale effects which may distinguish the gully and basin simulations are masked by the uncertainty in parameter evaluation.
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Published date: 1998
Identifiers
Local EPrints ID: 480388
URI: http://eprints.soton.ac.uk/id/eprint/480388
ISSN: 0144-7815
PURE UUID: f2d72479-e5ee-42b1-a3b9-289d06d985a9
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Date deposited: 01 Aug 2023 21:39
Last modified: 11 May 2024 01:48
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Contributors
Author:
James C. Bathurst
Author:
Ben Lukey
Author:
Robert A. Hiley
Author:
Nicolle Mathys
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