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Transverse transport of suspended sediment across the main channel – floodplain shear boundary

Thesis (MScEng (Civil Engineering))--University of Stellenbosch, 2006.

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Main Author: Denys, Frank
Other Authors: Basson, G. R.
Format: Thesis
Language:en_ZA
Published: Stellenbosch : University of Stellenbosch 2007
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access_status_str Open Access
author Denys, Frank
author2 Basson, G. R.
author_browse Basson, G. R.
Denys, Frank
author_facet Basson, G. R.
Denys, Frank
author_sort Denys, Frank
collection Thesis
dc_rights_str_mv University of Stellenbosch
description Thesis (MScEng (Civil Engineering))--University of Stellenbosch, 2006.
format Thesis
id oai:scholar.sun.ac.za:10019.1/2602
institution Stellenbosch University (South Africa)
language en_ZA
last_indexed 2026-06-10T12:44:06.995Z
license_str Other — see source repository
provenance_str_mv Harvested via OAI-PMH from SUNScholar — Stellenbosch University Repository
publishDate 2007
publishDateRange 2007
publishDateSort 2007
publisher Stellenbosch : University of Stellenbosch
publisherStr Stellenbosch : University of Stellenbosch
record_format dspace
source_str SUNScholar — Stellenbosch University Repository
spelling oai:scholar.sun.ac.za:10019.1/2602 Transverse transport of suspended sediment across the main channel – floodplain shear boundary Denys, Frank Basson, G. R. University of Stellenbosch. Faculty of Engineering. Dept. of Civil Engineering. Theses -- Civil engineering Dissertations -- Civil engineering Suspended sediments Sediment transport Floodplains Civil engineering Thesis (MScEng (Civil Engineering))--University of Stellenbosch, 2006. The floodplain of a river forms a close relationship with the stream that created it. Not only does the river influence the characteristics of the floodplain, the floodplain can also very easily influence its river, as is evidenced by examples such as the Huang He River in China and the Columbia River in Canada. These two cases clearly indicate that suspended sediment has a pronounced influence on the floodplain. This thesis investigates the processes which cause sediment to move onto the floodplain. As observed in many rivers worldwide suspended sediment on the floodplain has a tendency to settle near but not directly next to the main river channel. This gap between the river channel and the location of highest sedimentation rate stems from the fact that there is a zone of relatively higher turbulence at the boundaries of the floodplain. Close to this zone flow on the floodplain is increased in velocity whilst the flow velocity in the main channel is decreased as can be seen in the figure below: ... 2007-11-27T12:56:26Z 2010-06-01T08:53:25Z 2007-11-27T12:56:26Z 2010-06-01T08:53:25Z 2006-12 Thesis http://hdl.handle.net/10019.1/2602 en_ZA University of Stellenbosch 5141232 bytes application/pdf application/pdf Stellenbosch : University of Stellenbosch
spellingShingle Theses -- Civil engineering
Dissertations -- Civil engineering
Suspended sediments
Sediment transport
Floodplains
Civil engineering
Denys, Frank
Transverse transport of suspended sediment across the main channel – floodplain shear boundary
title Transverse transport of suspended sediment across the main channel – floodplain shear boundary
title_full Transverse transport of suspended sediment across the main channel – floodplain shear boundary
title_fullStr Transverse transport of suspended sediment across the main channel – floodplain shear boundary
title_full_unstemmed Transverse transport of suspended sediment across the main channel – floodplain shear boundary
title_short Transverse transport of suspended sediment across the main channel – floodplain shear boundary
title_sort transverse transport of suspended sediment across the main channel floodplain shear boundary
topic Theses -- Civil engineering
Dissertations -- Civil engineering
Suspended sediments
Sediment transport
Floodplains
Civil engineering
url http://hdl.handle.net/10019.1/2602
work_keys_str_mv AT denysfrank transversetransportofsuspendedsedimentacrossthemainchannelfloodplainshearboundary