Abstract
The present study concentrates mainly on the influence of sediment gradation on the wave-induced sediment transport and can be considered as a logical next step in an ongoing line of cross-shore sand transport research. The study focuses at improving our basic understanding of size-graded and uniform sand transport mechanisms in
cross-shore direction under oscillatory sheet-flow conditions. Sheet-flow is the dominant transport mode during storm conditions, when coastal and seabed erosion and deposition processes are generally very strong.
Original language | English |
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Qualification | Doctor of Philosophy |
Awarding Institution |
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Supervisors/Advisors |
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Award date | 7 May 2003 |
Place of Publication | Enschede |
Publisher | |
Print ISBNs | 90-365-1889-x |
Publication status | Published - 7 May 2003 |
Keywords
- IR-41433
- METIS-212879