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This document summarizes a study on the interaction between oscillatory boundary-layer flow induced by Faraday waves and a sedimentary granular layer in a vertically vibrated Hele-Shaw cell. The researchers observed a transition between a flat motionless granular layer and a regime where the layer undulates and oscillates periodically above a critical depth of the supernatant fluid layer. They found that the reduced acceleration needed for motion depends on particle diameter and depth, and that the wave vel

Author

Alejandro FT

Language

EN