All Stories

  1. Coevolving aerodynamic and impact ripples on Earth
  2. The role of hydrodynamics for the spatial distribution of high-temperature hydrothermal vent-endemic fauna in the deep ocean environment
  3. Influence of slope angle on deposit morphology and propagation of laboratory landslides
  4. Scaling laws for planetary sediment transport from DEM-RANS numerical simulations
  5. Anomalous Scaling of Aeolian Sand Transport Reveals Coupling to Bed Rheology
  6. Shear thinning of non-Brownian suspensions and its variation at different ambient conditions
  7. Turbidity currents propagating down an inclined slope: particle auto-suspension
  8. Copebot: Underwater Soft Robot with Copepod-Like Locomotion
  9. Thermohaline Dynamics in the Northern Continental Slope of the South China Sea: A Case Study in the Qiongdongnan Slope
  10. Fluid-particle interaction regimes during the evolution of turbidity currents from a coupled LES/DEM model
  11. Megaripple mechanics: bimodal transport ingrained in bimodal sands
  12. Aeolian sand transport: Scaling of mean saltation length and height and implications for mass flux scaling
  13. Unified model of sediment transport threshold and rate across weak and intense subaqueous bedload, windblown sand, and windblown snow
  14. Unification of Aeolian and Fluvial Sediment Transport Rate from Granular Physics
  15. The physics of sediment transport initiation, cessation, and entrainment across aeolian and fluvial environments
  16. The effect of turbulence on drifting snow sublimation
  17. Large Effects of Particle Size Heterogeneity on Dynamic Saltation Threshold
  18. Local Rheology Relation with Variable Yield Stress Ratio across Dry, Wet, Dense, and Dilute Granular Flows
  19. Comment on “Distinct Thresholds for the Initiation and Cessation of Aeolian Saltation From Field Measurements” by Raleigh L. Martin and Jasper F. Kok: Alternative Interpretation of Measured Thresholds as Two Distinct Cessation Thresholds
  20. Front Velocity and Front Location of Lock-Exchange Gravity Currents Descending a Slope in a Linearly Stratified Environment
  21. Universal friction law at granular solid-gas transition explains scaling of sediment transport load with excess fluid shear stress
  22. The Critical Role of the Boundary Layer Thickness for the Initiation of Aeolian Sediment Transport
  23. The cessation threshold of non-suspended sediment transport across environments
  24. Fluid forces or impacts: What governs the entrainment of soil particles in sediment transport mediated by a Newtonian fluid?
  25. Limitations of empirical sediment transport formulas for shallow water and their consequences for swash zone modelling
  26. An optimized dispersion–relation-preserving combined compact difference scheme to solve advection equations
  27. Modeling of Breaching Due to Overtopping Flow and Waves Based on Coupled Flow and Sediment Transport
  28. Is it appropriate to model turbidity currents with the three-equation model?
  29. Discrete Element Method simulations of the saturation of aeolian sand transport
  30. Well-balanced and flexible morphological modeling of swash hydrodynamics and sediment transport
  31. Electric Field and Humidity Trigger Contact Electrification
  32. The fluctuation energy balance in non-suspended fluid-mediated particle transport
  33. Analytical model for flux saturation in sediment transport
  34. Flux Saturation Length of Sediment Transport
  35. Midair Collisions Enhance Saltation
  36. The apparent roughness of a sand surface blown by wind from an analytical model of saltation
  37. Jump at the Onset of Saltation
  38. Why do particle clouds generate electric charges?