Two-dimensional mobile-bed dam-break model

Sudden and catastrophic dam-breaks typically induce high bed shear stresses downstream as the flood-wave propagates over the alluvial channel and flood plain. In fact, the non-dimensionalized shear stresses are often high enough that they are comparable to those typically seen in the transport of sa...

Full description

Bibliographic Details
Main Author: Tang, Gaven
Language:English
Published: University of British Columbia 2012
Online Access:http://hdl.handle.net/2429/43508
id ndltd-LACETR-oai-collectionscanada.gc.ca-BVAU.-43508
record_format oai_dc
spelling ndltd-LACETR-oai-collectionscanada.gc.ca-BVAU.-435082013-06-05T04:21:04ZTwo-dimensional mobile-bed dam-break modelTang, GavenSudden and catastrophic dam-breaks typically induce high bed shear stresses downstream as the flood-wave propagates over the alluvial channel and flood plain. In fact, the non-dimensionalized shear stresses are often high enough that they are comparable to those typically seen in the transport of sand. Despite the existence of these shear stresses, industry typically ignores sediment transport altogether and assumes a fixed-bed when modelling dam-breaks. This thesis will examine the validity of the fixed-bed assumption and create a depth-averaged 2D mobile-bed dam-break model. This model will then be tested by simulating the Malpasset (France) dam-break of 1959, and a sensitivity analysis will then be performed on the parameters of grain roughness, vegetation roughness, friction angle, grain size, and depth to bedrock to examine differences in inundation and flood-wave propagation.University of British Columbia2012-10-19T19:16:16Z2012-10-19T19:16:16Z20122012-10-192012-11Electronic Thesis or Dissertationhttp://hdl.handle.net/2429/43508eng
collection NDLTD
language English
sources NDLTD
description Sudden and catastrophic dam-breaks typically induce high bed shear stresses downstream as the flood-wave propagates over the alluvial channel and flood plain. In fact, the non-dimensionalized shear stresses are often high enough that they are comparable to those typically seen in the transport of sand. Despite the existence of these shear stresses, industry typically ignores sediment transport altogether and assumes a fixed-bed when modelling dam-breaks. This thesis will examine the validity of the fixed-bed assumption and create a depth-averaged 2D mobile-bed dam-break model. This model will then be tested by simulating the Malpasset (France) dam-break of 1959, and a sensitivity analysis will then be performed on the parameters of grain roughness, vegetation roughness, friction angle, grain size, and depth to bedrock to examine differences in inundation and flood-wave propagation.
author Tang, Gaven
spellingShingle Tang, Gaven
Two-dimensional mobile-bed dam-break model
author_facet Tang, Gaven
author_sort Tang, Gaven
title Two-dimensional mobile-bed dam-break model
title_short Two-dimensional mobile-bed dam-break model
title_full Two-dimensional mobile-bed dam-break model
title_fullStr Two-dimensional mobile-bed dam-break model
title_full_unstemmed Two-dimensional mobile-bed dam-break model
title_sort two-dimensional mobile-bed dam-break model
publisher University of British Columbia
publishDate 2012
url http://hdl.handle.net/2429/43508
work_keys_str_mv AT tanggaven twodimensionalmobilebeddambreakmodel
_version_ 1716588411823849472