This paper presents the effects of grain size and bottom slope on the longshore sand transport in the coastal zone (surf zone). Field data sets of sand transport in rivers, estuaries and coastal seas have been analysed to determine the effect of grain size. Three bulk-type formulae of longshore transport have been used to compute the longshore transport for a range of offshore wave conditions. Finally, a detailed cross-shore profile model (UNIBEST-TC of Delft Hydraulics) has been used to determine these effects for a new land reclamation site near the Port of Rotterdam, The Netherlands
This study investigates the relationship between grain-size distributions and sediment transport pro...
Longshore sediment transport (LST) is one of the main drivers of beach morphology. Bulk LST formulas...
Suspended sand is sampled at several heights and positions on a beach and foredune, providing detail...
Theory for across-shore transport as a function of beach slope and sediment size is extended to long...
The longshore sediment transport (it will be referred also as LST) is a core issue in the field of c...
Existing models for longshore sediment transport rate computations assume the sediment grain size an...
The response of longshore sediment transport to the morphodynamic state of the beach was assessed wi...
In the present SBEACH model, the effective grain size can range from 0.13 to 1.0 mm. The grain size ...
The area of interest in this study is the closed part of the Holland coast. This is the coastal stre...
Impact of spatial variability in the nearshore bathymetry on net sediment transport rates has been i...
The present study investigates longshore sediment transport for a variety of bathymetric and wave co...
Impact of spatial variability in the nearshore bathymetry on net sediment transport rates has been i...
Accurate predictions of the total rate of longshore sand transport (LST) and its cross-shore distrib...
This study investigates grain-size sorting through longshore transport processes and how it influenc...
Longshore Sediment Transport (LST) is one of the main drivers of beach morphology. It works at tempo...
This study investigates the relationship between grain-size distributions and sediment transport pro...
Longshore sediment transport (LST) is one of the main drivers of beach morphology. Bulk LST formulas...
Suspended sand is sampled at several heights and positions on a beach and foredune, providing detail...
Theory for across-shore transport as a function of beach slope and sediment size is extended to long...
The longshore sediment transport (it will be referred also as LST) is a core issue in the field of c...
Existing models for longshore sediment transport rate computations assume the sediment grain size an...
The response of longshore sediment transport to the morphodynamic state of the beach was assessed wi...
In the present SBEACH model, the effective grain size can range from 0.13 to 1.0 mm. The grain size ...
The area of interest in this study is the closed part of the Holland coast. This is the coastal stre...
Impact of spatial variability in the nearshore bathymetry on net sediment transport rates has been i...
The present study investigates longshore sediment transport for a variety of bathymetric and wave co...
Impact of spatial variability in the nearshore bathymetry on net sediment transport rates has been i...
Accurate predictions of the total rate of longshore sand transport (LST) and its cross-shore distrib...
This study investigates grain-size sorting through longshore transport processes and how it influenc...
Longshore Sediment Transport (LST) is one of the main drivers of beach morphology. It works at tempo...
This study investigates the relationship between grain-size distributions and sediment transport pro...
Longshore sediment transport (LST) is one of the main drivers of beach morphology. Bulk LST formulas...
Suspended sand is sampled at several heights and positions on a beach and foredune, providing detail...