Page 3: 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.

Up to 4,700 metric tons of litter flows down the Rhine each year

The river Rhine is estimated to carry between 3,000 and 4,700 metric tons of macrolitter—pieces of litter larger than 25 millimeters in size—towards the North Sea every year, according to research published in Communications ...

The shape of sand grains reveals the distance traveled by rivers

A team from the Centro Nacional de Investigación sobre la Evolución Humana (CENIEH) has collaborated with researchers from the University of Málaga (UMA) and the University of Córdoba (UCO) on an article published in the ...

Boulder washed inland a sign of Pacific tsunami history

Analysis has shown a boulder weighing almost 1,200 tons in Tonga is one of the largest known wave-transported rocks in the world, providing new insights into the Pacific region's history and risk of tsunamis.

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