Please use this identifier to cite or link to this item:
Title: Sheet flow layer structure under oscillatory flows
Authors: Silva, P. A.
Abreu, T.
Michallet, H.
Hurther, D.
Sancho, F. E.
Issue Date: 2009
Abstract: Under large near-bed oscillatory velocities, sediment transport mainly occurs within a thin layer, known as the sheet flow layer. The structure of the sheet flow layer changes along the wave cycle, with maximum thickness around maximum onshore and off-shore velocities and minima at flow reversals. These changes are intimately related to the lower and upper bounds of the sheet flow layer. In the present work, the intra-wave changes of the sheet flow thickness for oscillatory flows, with acceleration and velocity skewnesses, are analysed based on detailed measurements of the sediment concentration within the bed layer and the backscattered signal of an Acoustic Doppler Velocity Profiler, located above. The results from both measurements are compared and discussed as a function of the physical forcing parameters: net current, flow acceleration and velocity skewnesses.
Appears in Collections:DHA/NEC - Comunicações a congressos e artigos de revista

Files in This Item:
File Description SizeFormat 
Silva-et-al_RCEM-Final.pdf344.12 kBAdobe PDFView/Open

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.