The erosion threshold, beyond which bed sediments start to move, is a key parameter
describing sediment transport processes. For silt‐dominated mixtures, in which the grain …

The factors influencing pore pressure and the reason there was no residual liquefaction are
discussed. The effects of pore water pressure response are mainly determined by the …

A double-layer transverse oscillating grid for a flume was designed and manufactured, in
order to generate approximately isotropic homogeneous turbulence, and allowing the effect …

The prediction of the erosion of mudflats is hampered by inaccurate estimates of the
erodibility distribution of the sediment bed. To investigate how erodibility varies in space and …

The radial sand ridges consist of more than 70 sand ridges that are spread out radially on
the continental shelf of the South Yellow Sea. As a unique geomorphological feature in the …

The main purpose of the research was to develop appropriate tools for forecasting the
effects of storms. The use of the high-resolution SWAN wave model powered by AROME …

Water resource pollution, particularly in river channels, presents a grave environmental
challenge that necessitates a comprehensive and systematic approach encompassing …

In this study, we aim to investigate the overall morphological evolution of the Jiangsu coast
after 1855, when the Yellow River shifted northward. We focus on fine sediment transport …

Residual sediment transport, which is influenced by many factors including tide, wind, and
waves, controls coastal morphological changes on different time scales. For fine-grained …

Sediment incipient motion is a fundamental issue in sediment transport theory and
engineering practice. Silt has transitional behavior between cohesive and non-cohesive …