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Entrainment from a bed of particles by thermal convection
Viatcheslav S. Solomatov
, Peter Olson
, David J. Stevenson
Department of Earth & Planetary Sciences
Research output
:
Contribution to journal
›
Article
›
peer-review
63
Scopus citations
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Keyphrases
Entrainment
100%
Thermal Convection
100%
Convection
28%
Earth's Core
28%
Magma Chamber
28%
Re-entrainment
14%
Competition Process
14%
Particle Bed
14%
Early Earth
14%
Turbulent Regime
14%
Dunes
14%
Small Crystals
14%
Simple Theory
14%
Suspended Solids
14%
Viscous Stress
14%
Laminar Regime
14%
Magma Ocean
14%
Partially Molten
14%
High Rayleigh number
14%
Convective Layer
14%
Thermal Plume
14%
Dune Formation
14%
Large Viscosity
14%
Convecting Fluid
14%
Reynolds Stress
14%
Solid Fraction
14%
Earth and Planetary Sciences
Earth Core
100%
Magma Chamber
100%
Free Convection
100%
Early Earth
50%
Magma
50%
Fluidised Bed
50%
Rayleigh Number
50%
Dune Formation
50%
Chemical Engineering
Fluidized Bed
100%
Suspended Particulate Matter
100%
Reentrainment
100%
Thermal Plume
100%