Research news on sediment transport

Sediment transport is the suite of physical processes governing the entrainment, movement, and deposition of particulate material (clastic or biogenic) by a transporting medium, typically water, air, or ice. In fluvial and coastal systems, it is controlled by fluid shear stress, turbulence, grain size, density, and bed roughness, and occurs as bedload, suspended load, or wash load. Sediment transport underpins channel and shoreline morphodynamics, stratigraphic architecture, and landscape evolution, and is commonly quantified using transport equations (e.g., Shields parameter–based formulations) and numerical models that couple hydrodynamics with sediment entrainment, advection, diffusion, and deposition.

Measuring massive surge waves along the Illgraben

Researchers at the Swiss Federal Institute for Forest, Snow and Landscape Research (WSL) have, for the first time, been able to record a debris flow over a distance of two kilometers at the Illgraben (VS). The study reveals ...

Were Martian tides strong enough to shape its ancient landscape?

You're an anaerobic microbe sunbathing on a Martian beach billions of years ago listening to the small waves hit the shoreline as you take in the perchlorates in the Martian regolith. This is because while Mars is warm and ...

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