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Published on: December 4, 2017
Two-dimensional granular Poiseuille flow on an incline: multiple dynamical regimes
1Department of Physics and Astronomy, Haverford College, Haverford, Pennsylvania 19041, USA.
Granular flows in channels transition between dilute and dense states. Constricted exits enable steady flow, while rough sidewalls are crucial for oscillatory two-phase flow, revealing complex particle dynamics.
Area of Science:
- Experimental physics
- Granular flow dynamics
- Soft matter physics
Background:
- Understanding granular flow is crucial in various industrial and geophysical processes.
- Previous studies often simplified channel boundaries or flow conditions, limiting applicability.
- The role of sidewall roughness and exit geometry in granular flow behavior remains underexplored.
Purpose of the Study:
- To experimentally investigate the flow of granular materials in a confined channel with specific boundary conditions.
- To characterize the flow regimes and particle dynamics under varying exit conditions and channel geometries.
- To identify the influence of rough sidewalls on granular flow patterns.
Main Methods:
- Utilized high-speed video imaging for precise particle tracking.
- Quantified particle positions and velocities in a monolayer flow down an inclined channel.
- Varied channel exit conditions (open vs. constricted) and sidewall properties (smooth vs. rough).
Main Results:
- Open exits resulted in accelerating, dilute flows.
- Constricted exits led to steady-state flows with a continuous transition between oscillatory two-phase flow (2PF) and uniform dense flow.
- Rough sidewalls were essential for the 2PF regime, characterized by distinct density variations, temporal regularity, and transverse profiles; dense regions showed arches and lattice structures, while dilute regions were nearly collisionless.
Conclusions:
- Granular flow behavior is highly sensitive to confinement geometry, particularly sidewall roughness and exit conditions.
- The study identified distinct flow regimes (2PF and dense flow) with unique particle dynamics, driven by confinement.
- Current models are insufficient to capture the full complexity of these granular flows, including the transition between dense and dilute regions.
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