Sediments are periodically dredged from the major ports in the Gulf of Gabes (GG) during
maintenance operations. These sediments are dumped near the coats of Sfax and Gabes …

Wave nonlinearity is a main driving force for near-bed sediment transport, and thus affects
the beach evolution. Accurate prediction of wave nonlinearity is an essential need for the …

The morphology of tide‐dominated systems is progressively influenced by human activities
and climate change. Quantitative approaches aiming at understanding or forecasting the …

The sediment composition of the seabed governs its mobility, hence determining sediment
transport and morphological evolution of estuaries and tidal basins. Bed sediments often …

Pyroclastic density currents (PDCs) are hazardous, multiphase currents of heterogeneous
volcanic material and gas. Moisture (as liquid or gas) can enter a PDC through external (eg …

Relatively little is known about the geomorphological characteristics of floodplain secondary
channels and the potential for floodplain flows to mobilize bed material within these …

Significant advancements have been made in understanding local scour around pile
foundations in non-cohesive soils; however, the scour phenomenon in clay soils remains …

Cohesive sediment is ubiquitous in aquatic systems, which often forms fractal aggregates
due to cohesive and adhesive forces between particles and is generally eroded as …

Simulating sediment dynamics in a large and energetic estuary system remains challenging,
primarily due to the spatial and temporal complexities of the interaction between flow and …

Sediment with varying sizes is transported through runoff, finding ways into sewerage pipes
and deposited at low-velocity sections. As wastewater is high in organic content, biofilm …