Synergistic cavitation–particle erosion often occurs in high-speed sediment-laden flow in
hydraulic structures and machines. However, erosion prediction is challenging due to the …

Lateral erosion is a critical factor that influences the formation and amplification of debris
flows. However, our understanding of the bank retreat process in debris flow channels is …

The dynamics of suspended particulate matter (SPM) and SPM‐associated biological and
physicochemical processes in a river vary under dry and wet weather conditions and …

In this study, the incipient motion thresholds of coral sediment with the action of oscillatory
currents were experimentally recorded by conducting a total of 405 laboratory experiments …

The flocculation of cohesive sediment particles is a function of the collision efficiency of
sediment particles, which is mainly influenced by local flow hydrodynamics. A detailed study …

Biofilm surrounding sediment particles can significantly enhance the stability of coastal
sediment. This phenomenon is known as biostabilization. Biofilm mainly consists of …

Clay is the main component that contributes to sediment cohesiveness. Salinity impacts its
transport, which controls the electrochemical force among the sediment grains. Here, we …

The initiation threshold of sediment motion, a key component in quantifying sediment
transport, has potential link to intermittent turbulence bursts. Here, we elaborated in situ …

Estuarine deltas play a critical role in the interaction between the ocean and land and serve
as the primary location for the deposition of terrestrial organic carbon and pollutants …

The effect of mean flow velocity on phosphorus (P) partitioning between water and sediment
has received much attention in recent decades. However, the impact of turbulence on the …