Velocity correlations in dense granular flows
Olivier Pouliquen (IUSTI)

TL;DR
This study experimentally investigates velocity fluctuations in dense granular flows on inclined planes, revealing a correlation length influenced by inclination angle, suggesting flow dynamics are governed by a characteristic length scale larger than individual grains.
Contribution
It demonstrates that the velocity correlation length in dense granular flows depends on inclination angle, not layer thickness, highlighting a characteristic length scale beyond individual particles.
Findings
Correlation length depends on inclination angle
Velocity fluctuations are correlated over a few grain diameters
Flow dynamics are governed by a characteristic length larger than a single grain
Abstract
Velocity fluctuations of grains flowing down a rough inclined plane are experimentally studied. The grains at the free surface exhibit fluctuating motions, which are correlated over few grains diameters. The characteristic correlation length is shown to depend on the inclination of the plane and not on the thickness of the flowing layer. This result strongly supports the idea that dense granular flows are controlled by a characteristic length larger than the particle diameter.
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Taxonomy
TopicsGranular flow and fluidized beds · Landslides and related hazards · Hydrology and Sediment Transport Processes
