All Stories

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