Interaction of a granular stream with an obstacle
Volkhard Buchholtz, Thorsten Poeschel

TL;DR
This study numerically examines how a granular stream interacts with an obstacle, revealing different force behaviors at high and low velocities, including a gas-filled gap formation at low velocities.
Contribution
It provides new insights into the velocity-dependent forces and gap formation in granular streams impacting obstacles, highlighting a transition from quadratic to different force laws.
Findings
Force proportional to velocity squared at high speeds
Gap formation with granular gas at low speeds
Different force laws depending on stream velocity
Abstract
We investigate numerically the interaction of a stream of granular particles with a resting obstacle in two dimensions. For the case of high stream velocity we find that the force acting on the obstacle is proportional to the square of the stream velocity, the density and the obstacle size. This behavior is equivalent to that of non- interacting hard spheres. For low stream velocity there appears a gap in between the obstacle and the incoming stream particles which is filled with granular gas of high temperature and low density. As soon as the gap appears the force does not depend on the square of velocity of the stream but the dependency obeys another law.
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Taxonomy
TopicsGranular flow and fluidized beds · Landslides and related hazards · Particle Dynamics in Fluid Flows
