Consolidation of Non-Colloidal Spherical Particles at Low Particle Reynolds Numbers

When a system of identical spheres settles under conditions of negligible surface and inertial forces an idealised form of sediment consolidation unfolds amenable to a universal description. We have described this complex process using a simple constitutive model expressed as an elementary scaling l...

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Main Authors: Kevin P. Galvin, Marveh Forghani, Elham Doroodchi, Simon M. Iveson
Format: Article
Language:English
Published: Hosokawa Powder Technology Foundation 2015-07-01
Series:KONA Powder and Particle Journal
Subjects:
Online Access:https://www.jstage.jst.go.jp/article/kona/33/0/33_2016006/_html/-char/en
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spelling doaj-595989296b314379be87f5e81bed59be2021-02-03T00:48:56ZengHosokawa Powder Technology FoundationKONA Powder and Particle Journal0288-45342187-55372015-07-0133024926310.14356/kona.2016006konaConsolidation of Non-Colloidal Spherical Particles at Low Particle Reynolds NumbersKevin P. Galvin0Marveh Forghani1Elham Doroodchi2Simon M. Iveson3Centre for Advanced Particle Processing and Transport, Newcastle Institute for Energy and Resources, The University of Newcastle, AustraliaCentre for Advanced Particle Processing and Transport, Newcastle Institute for Energy and Resources, The University of Newcastle, AustraliaCentre for Advanced Particle Processing and Transport, Newcastle Institute for Energy and Resources, The University of Newcastle, AustraliaCentre for Advanced Particle Processing and Transport, Newcastle Institute for Energy and Resources, The University of Newcastle, AustraliaWhen a system of identical spheres settles under conditions of negligible surface and inertial forces an idealised form of sediment consolidation unfolds amenable to a universal description. We have described this complex process using a simple constitutive model expressed as an elementary scaling law in time, t, applied at the local particle level. The free-volume surrounding a particle consists of two volume contributions occupied by fluid, one portion fixed and the other portion variable, the latter of which declines with t−2. A comprehensive system of analytical equations was derived using this one idea, and associated boundary conditions, to describe all aspects of the batch settling process. An experimental system exhibiting negligible surface and inertial forces was used to validate the model and hence assess the merits of the scaling law. Excellent agreement was achieved. The precise physics responsible for this scaling law, and the applicable boundary conditions, remain unclear at this stage. Hence this work is likely to motivate further work in this area, concerned with the dynamics of random consolidation of settling spheres.https://www.jstage.jst.go.jp/article/kona/33/0/33_2016006/_html/-char/ensedimentationconsolidationscaling lawsnon-colloidal sphereslow reynolds number
collection DOAJ
language English
format Article
sources DOAJ
author Kevin P. Galvin
Marveh Forghani
Elham Doroodchi
Simon M. Iveson
spellingShingle Kevin P. Galvin
Marveh Forghani
Elham Doroodchi
Simon M. Iveson
Consolidation of Non-Colloidal Spherical Particles at Low Particle Reynolds Numbers
KONA Powder and Particle Journal
sedimentation
consolidation
scaling laws
non-colloidal spheres
low reynolds number
author_facet Kevin P. Galvin
Marveh Forghani
Elham Doroodchi
Simon M. Iveson
author_sort Kevin P. Galvin
title Consolidation of Non-Colloidal Spherical Particles at Low Particle Reynolds Numbers
title_short Consolidation of Non-Colloidal Spherical Particles at Low Particle Reynolds Numbers
title_full Consolidation of Non-Colloidal Spherical Particles at Low Particle Reynolds Numbers
title_fullStr Consolidation of Non-Colloidal Spherical Particles at Low Particle Reynolds Numbers
title_full_unstemmed Consolidation of Non-Colloidal Spherical Particles at Low Particle Reynolds Numbers
title_sort consolidation of non-colloidal spherical particles at low particle reynolds numbers
publisher Hosokawa Powder Technology Foundation
series KONA Powder and Particle Journal
issn 0288-4534
2187-5537
publishDate 2015-07-01
description When a system of identical spheres settles under conditions of negligible surface and inertial forces an idealised form of sediment consolidation unfolds amenable to a universal description. We have described this complex process using a simple constitutive model expressed as an elementary scaling law in time, t, applied at the local particle level. The free-volume surrounding a particle consists of two volume contributions occupied by fluid, one portion fixed and the other portion variable, the latter of which declines with t−2. A comprehensive system of analytical equations was derived using this one idea, and associated boundary conditions, to describe all aspects of the batch settling process. An experimental system exhibiting negligible surface and inertial forces was used to validate the model and hence assess the merits of the scaling law. Excellent agreement was achieved. The precise physics responsible for this scaling law, and the applicable boundary conditions, remain unclear at this stage. Hence this work is likely to motivate further work in this area, concerned with the dynamics of random consolidation of settling spheres.
topic sedimentation
consolidation
scaling laws
non-colloidal spheres
low reynolds number
url https://www.jstage.jst.go.jp/article/kona/33/0/33_2016006/_html/-char/en
work_keys_str_mv AT kevinpgalvin consolidationofnoncolloidalsphericalparticlesatlowparticlereynoldsnumbers
AT marvehforghani consolidationofnoncolloidalsphericalparticlesatlowparticlereynoldsnumbers
AT elhamdoroodchi consolidationofnoncolloidalsphericalparticlesatlowparticlereynoldsnumbers
AT simonmiveson consolidationofnoncolloidalsphericalparticlesatlowparticlereynoldsnumbers
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