Comparison of flow resistance relations for debris flows using a one-dimensional finite element simulation model

This paper describes a one-dimensional finite element code for debris flows developed to model the flow within a steep channel and the stopping conditions on the fan. The code allows the systematic comparison of a wide variety of previously proposed one-phase flow resistance laws using the same fini...

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Main Authors: D. Naef, D. Rickenmann, P. Rutschmann, B. W McArdell
Format: Article
Language:English
Published: Copernicus Publications 2006-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/6/155/2006/nhess-6-155-2006.pdf
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spelling doaj-ddd58c086fe242dea8b5632674cf787d2020-11-24T23:01:30ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812006-01-0161155165Comparison of flow resistance relations for debris flows using a one-dimensional finite element simulation modelD. NaefD. NaefD. RickenmannD. RickenmannP. RutschmannB. W McArdellThis paper describes a one-dimensional finite element code for debris flows developed to model the flow within a steep channel and the stopping conditions on the fan. The code allows the systematic comparison of a wide variety of previously proposed one-phase flow resistance laws using the same finite element solution method. The one-dimensional depth-averaged equations of motion and the numerical model are explained. The model and implementation of the flow resistance relations was validated using published analytical results for the dam break case. Reasonable agreement for the front velocities and stopping location for a debris-flow event in the Kamikamihori torrent in Japan can be achieved with turbulent flow resistance relations including 'stop' terms which allow the flow to come to rest on a gently sloping surface. While it is possible to match the overall bulk flow behavior using relatively simple flow resistance relations, they must be calibrated. A sensitivity analysis showed that the shape of the upstream input hydrograph does not much affect the flow conditions in the lower part of the flow path, whereas the event volume is much more important.http://www.nat-hazards-earth-syst-sci.net/6/155/2006/nhess-6-155-2006.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. Naef
D. Naef
D. Rickenmann
D. Rickenmann
P. Rutschmann
B. W McArdell
spellingShingle D. Naef
D. Naef
D. Rickenmann
D. Rickenmann
P. Rutschmann
B. W McArdell
Comparison of flow resistance relations for debris flows using a one-dimensional finite element simulation model
Natural Hazards and Earth System Sciences
author_facet D. Naef
D. Naef
D. Rickenmann
D. Rickenmann
P. Rutschmann
B. W McArdell
author_sort D. Naef
title Comparison of flow resistance relations for debris flows using a one-dimensional finite element simulation model
title_short Comparison of flow resistance relations for debris flows using a one-dimensional finite element simulation model
title_full Comparison of flow resistance relations for debris flows using a one-dimensional finite element simulation model
title_fullStr Comparison of flow resistance relations for debris flows using a one-dimensional finite element simulation model
title_full_unstemmed Comparison of flow resistance relations for debris flows using a one-dimensional finite element simulation model
title_sort comparison of flow resistance relations for debris flows using a one-dimensional finite element simulation model
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2006-01-01
description This paper describes a one-dimensional finite element code for debris flows developed to model the flow within a steep channel and the stopping conditions on the fan. The code allows the systematic comparison of a wide variety of previously proposed one-phase flow resistance laws using the same finite element solution method. The one-dimensional depth-averaged equations of motion and the numerical model are explained. The model and implementation of the flow resistance relations was validated using published analytical results for the dam break case. Reasonable agreement for the front velocities and stopping location for a debris-flow event in the Kamikamihori torrent in Japan can be achieved with turbulent flow resistance relations including 'stop' terms which allow the flow to come to rest on a gently sloping surface. While it is possible to match the overall bulk flow behavior using relatively simple flow resistance relations, they must be calibrated. A sensitivity analysis showed that the shape of the upstream input hydrograph does not much affect the flow conditions in the lower part of the flow path, whereas the event volume is much more important.
url http://www.nat-hazards-earth-syst-sci.net/6/155/2006/nhess-6-155-2006.pdf
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