Formation of cylindrical shells via sphere packing from fluidized beds

and 4.7. For given ranges of flow velocities and bed sizes, particles settle on the wall, with a decrease in the bed height and particle fluctuations. Either a glass- or crystal-like shell forms along the pipe wall, in qualitative agreement with previous experiments. The polydispersity and the particle-particle friction are varied to test the stability of the particulate shell formation. The shell structure is analyzed by unwrapping it in a plane and locating all particles and their contact points, and we find that it exhibits a hexagonal lattice with a defects density that increases with polydispersity. The shell formation is hindered by polydispersity, and there exists a critical point for polydispersity above which a crystal-like shell is unstable. In a particular case of bidisperse beds, the crystal-like shell only appears when the particle-particle friction is high enough. Finally, we compute the contact forces within particle-particle chains and in particle-wall contacts, which sustain the cylindrical shell, highlighting the dominant role of particle-particle forces.

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Publication Details

Journal
The European Physical Journal E
Published
2026-04-01
DOI
https://doi.org/10.1140/epje/s10189-026-00573-z
Primary Topic
Granular flow and fluidized beds
Type
article
Field-Weighted Citation Impact
0.00

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article

Formation of cylindrical shells via sphere packing from fluidized beds

Danilo S. Borges, Jorge Peixinho, Erick Franklin
The European Physical Journal E
Granular flow and fluidized beds
article

Formation of cylindrical shells via sphere packing from fluidized beds

Danilo S. Borges, Jorge Peixinho, Erick Franklin
article en

Abstract

and 4.7. For given ranges of flow velocities and bed sizes, particles settle on the wall, with a decrease in the bed height and particle fluctuations. Either a glass- or crystal-like shell forms along the pipe wall, in qualitative agreement with previous experiments. The polydispersity and the particle-particle friction are varied to test the stability of the particulate shell formation. The shell structure is analyzed by unwrapping it in a plane and locating all particles and their contact points, and we find that it exhibits a hexagonal lattice with a defects density that increases with polydispersity. The shell formation is hindered by polydispersity, and there exists a critical point for polydispersity above which a crystal-like shell is unstable. In a particular case of bidisperse beds, the crystal-like shell only appears when the particle-particle friction is high enough. Finally, we compute the contact forces within particle-particle chains and in particle-wall contacts, which sustain the cylindrical shell, highlighting the dominant role of particle-particle forces.

The European Physical Journal EVol. 49(4)
Centre National de la Recherche Scientifique (FR), Universidade Estadual de Campinas (UNICAMP) (BR), Arts et Métiers (FR), Stadtwerke Duisburg (Germany) (DE), Entwicklungszentrum für Schiffstechnik und Transportsysteme (DE), University of Duisburg-Essen (DE)
Fundação de Amparo à Pesquisa do Estado de São Paulo, Centre National de la Recherche Scientifique
Openalex Percentile: Top 28%
Granular flow and fluidized beds
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